Refine
Has Fulltext
- yes (508) (remove)
Year of publication
Document Type
- Doctoral Thesis (327)
- Postprint (139)
- Other (12)
- Conference Proceeding (10)
- Habilitation Thesis (6)
- Master's Thesis (6)
- Article (3)
- Bachelor Thesis (2)
- Report (2)
- Monograph/Edited Volume (1)
Keywords
- Seismologie (20)
- Erdbeben (19)
- climate change (19)
- remote sensing (17)
- Fernerkundung (15)
- Anden (12)
- Andes (12)
- Klimawandel (12)
- Tektonik (11)
- earthquake (11)
- tectonics (11)
- climate (10)
- erosion (10)
- seismology (10)
- Argentinien (9)
- Erosion (9)
- Geomorphologie (9)
- Paläoklima (9)
- Seismology (9)
- geomorphology (9)
- numerische Modellierung (9)
- Argentina (8)
- Geophysik (8)
- Himalaya (8)
- Holocene (8)
- Klima (8)
- Naturgefahren (8)
- Subduktion (8)
- permafrost (8)
- thermochronology (8)
- Geologie (7)
- Holozän (7)
- InSAR (7)
- Modellierung (7)
- Neotektonik (7)
- lake sediments (7)
- Magnetotellurik (6)
- Seesedimente (6)
- Thermochronologie (6)
- geology (6)
- geophysics (6)
- modelling (6)
- natural hazards (6)
- stable isotopes (6)
- Arrayseismologie (5)
- Biomarker (5)
- Bodenfeuchte (5)
- Central Andes (5)
- Geochemie (5)
- Geodynamik (5)
- Momententensor (5)
- Monsun (5)
- Paläoklimatologie (5)
- Permafrost (5)
- Seismotektonik (5)
- Tsunami (5)
- Zeitreihenanalyse (5)
- Zentralanden (5)
- array seismology (5)
- biomarker (5)
- geochronology (5)
- kosmogene Nuklide (5)
- moment tensor (5)
- neotectonics (5)
- palaeoclimate (5)
- seismic noise (5)
- site effects (5)
- soil moisture (5)
- subduction (5)
- subduction zone (5)
- temperature (5)
- time series analysis (5)
- Arktis (4)
- Central Asia (4)
- Chile (4)
- Deformation (4)
- Earthquake (4)
- Erdmantel (4)
- Geochronologie (4)
- Geothermie (4)
- Himalaja (4)
- Hochwasser (4)
- Inversion (4)
- Iran (4)
- Rheologie (4)
- Sedimentologie (4)
- Spektroskopie (4)
- Subduction (4)
- Subduktionszone (4)
- Tibetan Plateau (4)
- Vogtland (4)
- West Bohemia (4)
- floods (4)
- foreland basin (4)
- geochemistry (4)
- geodynamics (4)
- hyperspectral (4)
- imaging spectroscopy (4)
- induced seismicity (4)
- inversion (4)
- landslides (4)
- machine learning (4)
- monsoon (4)
- numerical modeling (4)
- numerical simulation (4)
- seismic hazard (4)
- simulation (4)
- stabile Isotope (4)
- water (4)
- Africa (3)
- Afrika (3)
- Arctic (3)
- Carbonate (3)
- Cosmogenic nuclides (3)
- East African Rift (3)
- East African Rift System (3)
- Erdrutsch (3)
- Georadar (3)
- Germany (3)
- Hydrologie (3)
- Kosmogene Nuklide (3)
- Lake Van (3)
- Lake sediments (3)
- Landschaftsentwicklung (3)
- Nachbeben (3)
- Optische Fernerkundung (3)
- PHREEQC (3)
- Paläolimnologie (3)
- Pollen (3)
- Rheology (3)
- Schadensmodellierung (3)
- Simulation (3)
- South America (3)
- Standorteffekte (3)
- Strukturgeologie (3)
- Südamerika (3)
- Vegetation (3)
- Zentralasien (3)
- arctic (3)
- carbon dioxide (3)
- climate-change (3)
- correlation (3)
- cosmogenic nuclides (3)
- damage (3)
- deep biosphere (3)
- deep learning (3)
- deformation (3)
- dynamics (3)
- events (3)
- exhumation (3)
- extension (3)
- extreme rainfall (3)
- faults (3)
- hydrologische Modellierung (3)
- hydrology (3)
- magnetotellurics (3)
- model (3)
- modeling (3)
- monitoring (3)
- numerical modelling (3)
- paleoclimate (3)
- plateau (3)
- record (3)
- runoff (3)
- seismisches Rauschen (3)
- seismotectonics (3)
- snow (3)
- soil organic carbon (3)
- spectroscopy (3)
- subsidence (3)
- suspended sediment (3)
- time-series (3)
- uncertainty (3)
- varved lake sediments (3)
- vegetation (3)
- warvierte Seesedimente (3)
- water balance (3)
- Abbildende Spektroskopie (2)
- Alborz (2)
- Alpen (2)
- Alps (2)
- Anisotropie (2)
- Anpassung (2)
- Antarktis (2)
- Aral Sea (2)
- Arava Fault (2)
- Arava-Störung (2)
- Arctic tundra (2)
- Argon (2)
- Array Seismology (2)
- Black Sea (2)
- Boden (2)
- Bodenbewegungsmodelle (2)
- Bodenhydrologie (2)
- Bodenunruhe (2)
- Bruchausbreitung (2)
- Carbo-Iron (2)
- Chinese loess (2)
- Climate (2)
- Climate change (2)
- Colombia (2)
- Dead Sea (2)
- Dead Sea Transform (2)
- Deformationsmechanismen (2)
- Denudation (2)
- Diatomeen (2)
- Dichtemodellierung (2)
- Diffusion (2)
- Earth's magnetic field (2)
- East Antarctica (2)
- Eastern Cordillera (2)
- Elbe (2)
- Elburs (2)
- EnMAP (2)
- Erdbebenkatalog (2)
- Erdbebenschwarm 2008/09 (2)
- Erdbebenschwärme (2)
- Erdbebenvorhersage (2)
- Erdmagnetfeld (2)
- Europa (2)
- Fluid (2)
- GIS (2)
- GITEWS (2)
- GNSS (2)
- GPS (2)
- Gashydrate (2)
- Gewässerfernerkundung (2)
- Gletscher (2)
- Gravity (2)
- HVSR (2)
- Hangrutschungen (2)
- Helium (2)
- Hochdruck (2)
- Hyperspektral (2)
- Indien (2)
- Indischer Ozean (2)
- Indonesia (2)
- Kalahari (2)
- Karbonat (2)
- Karbonate (2)
- Kern-Mantel Grenze (2)
- Klimarekonstruktion (2)
- Klimaänderung (2)
- Kohlenstoff (2)
- Kolumbien (2)
- Küstenerosion (2)
- LGM (2)
- Lagerstätte (2)
- Landnutzung (2)
- Landnutzungswandel (2)
- Landslide (2)
- Lithosphäre (2)
- Menderes Massif (2)
- Menderes Massiv (2)
- Methanhydrat (2)
- Migration (2)
- Miocene (2)
- Miozän (2)
- Momententensoren (2)
- Monsoon (2)
- NAO (2)
- Nanoeisen (2)
- Natural Hazards (2)
- Neon (2)
- Oberflächenprozesse (2)
- Opalinus Clay (2)
- Opalinuston (2)
- Orogen (2)
- Ostafrikanisches Grabensystem (2)
- Ostantarktis (2)
- Paleoclimatology (2)
- Paleoseismologie (2)
- Paläogeographie (2)
- Paläomagnetik (2)
- Paläoökologie (2)
- Pamir (2)
- Patagonia (2)
- Perm (2)
- Permian (2)
- Petrologie (2)
- Photogrammetrie (2)
- Photogrammetry (2)
- Pirquitas (2)
- Plateau (2)
- Puna (2)
- Quartär (2)
- Raman spectroscopy (2)
- Randelementmethode (2)
- Reflexionsseismik (2)
- Remote sensing (2)
- Rift (2)
- Risikokommunikation (2)
- Riss (2)
- SAR (2)
- SWIM (2)
- Sanierung (2)
- Schwarmbeben (2)
- Schwarzes Meer (2)
- Sedimentology (2)
- Sedimenttransport (2)
- Seen (2)
- Seesediment (2)
- Seitenverschiebung (2)
- Sentinel-1 (2)
- Siberia (2)
- Spannungsfeld (2)
- Stratigraphy (2)
- Tectonics (2)
- Thermokarst (2)
- Tibet Plateau (2)
- Tien Shan (2)
- Totes Meer Störungssystem (2)
- Tropen (2)
- UAV (2)
- Uncertainties (2)
- Unsicherheiten (2)
- Unsicherheitsanalyse (2)
- Verwerfungen (2)
- Vogtland/West Bohemia (2)
- Vogtland/Westböhmen (2)
- Vorhersage (2)
- Vorlandbecken (2)
- Vulkan (2)
- Vulnerabilität (2)
- Warven (2)
- Wasser (2)
- Wasserhaushalt (2)
- Wetterlagen (2)
- Wärmeleitfähigkeit (2)
- agriculture (2)
- anisotropy (2)
- arktische Tundra (2)
- attenuation tomography (2)
- carbon (2)
- classification (2)
- climate extremes (2)
- climate variability (2)
- coast (2)
- coastal erosion (2)
- coherence (2)
- crust (2)
- damage modeling (2)
- deep convection (2)
- diffusion (2)
- digital rock physics (2)
- displacement (2)
- earthquake catalog (2)
- earthquake interaction (2)
- earthquake modeling (2)
- earthquake swarm (2)
- earthquake swarm 2008/09 (2)
- earthquake swarms (2)
- earthquakes (2)
- eastern south–central Andes (2)
- eclogite (2)
- ecological modelling (2)
- ecosystems (2)
- electrical conductivity (2)
- elektrische Leitfähigkeit (2)
- event coincidence analysis (2)
- event synchronization (2)
- extreme events (2)
- flood risk (2)
- fluid flow (2)
- forecasting (2)
- geothermal energy (2)
- governance (2)
- hydraulic fracturing (2)
- hydrological modelling (2)
- hyporheic zone (2)
- hyporheische Zone (2)
- impacts (2)
- inverse theory (2)
- isotopes (2)
- karst (2)
- komplexes Netzwerk (2)
- lake (2)
- lake-level change (2)
- lakes (2)
- land use change (2)
- landscape evolution (2)
- landslide (2)
- lithosphere (2)
- local structure (2)
- lokale Struktur (2)
- mantle plumes (2)
- marine Terrassen (2)
- maschinelles Lernen (2)
- methane hydrate (2)
- micro-CT (2)
- microbial activity (2)
- microbial communities (2)
- mitigation (2)
- models (2)
- natural hazard (2)
- northern high latitudes (2)
- numerical model (2)
- numerische Simulation (2)
- ocean color remote sensing (2)
- oxygen (2)
- paleoclimatology (2)
- paleoecology (2)
- paleomagnetism (2)
- paleoseismology (2)
- photogrammetry (2)
- playa (2)
- precipitation (2)
- preparedness (2)
- radiocarbon (2)
- rare earth elements (2)
- reactive transport (2)
- reaktiver Transport (2)
- rifting (2)
- risk communication (2)
- salt pan (2)
- scale (2)
- seismic risk (2)
- seismic tomography (2)
- seismische Gefährdung (2)
- seismisches Risiko (2)
- signal propagation (2)
- soil (2)
- source inversion (2)
- spectral analysis (2)
- strain localization (2)
- streamflow (2)
- stress field (2)
- strike-slip fault (2)
- structural geology (2)
- surface heat flow (2)
- surface processes (2)
- tectonic geomorphology (2)
- tektonische Geomorphologie (2)
- thermal field (2)
- thermal modeling (2)
- thermische Modellierung (2)
- thermokarst (2)
- time series (2)
- trace elements (2)
- tropics (2)
- uncertainty analysis (2)
- uplift (2)
- variability (2)
- varves (2)
- vulnerability (2)
- wavelet (2)
- "Little Ice Age' (LIA) (1)
- "Medieval Warm Period' (MWP) (1)
- (Alters-) Datierungen (1)
- 26Al/10Be cosmogenic radionuclides (1)
- 26Al/10Be kosmogene Radionuklide (1)
- 2D Numerical Modelling (1)
- 2D tomography (1)
- 3-D Modellierung (1)
- 3-D outcrop modeling (1)
- 3D (1)
- 3D Finite Element (1)
- 3D geomechanical numerical model (1)
- 3D geomechanisch-nummerische Modellierung (1)
- 3D numerical models (1)
- 3D numerische Modelle (1)
- 3D printing (1)
- 40Ar-39Ar Datierungsmethode (1)
- 40Ar/39Ar (1)
- ALOS World 3D (1)
- ALOS/PALSAR (1)
- ASM (1)
- ASPECT (1)
- ASTER GDEM (1)
- ASTER Satellitendaten (1)
- ASTER satellite images (1)
- Abbaufrontkartierung (1)
- Abschiebungshorizonte (1)
- Abschätzung der Unsicherheiten (1)
- Absorptionseigenschaften (1)
- Accuracy Asseessment (1)
- Accuracy Assessment (1)
- Acidithiobacillus (1)
- Acidobactetiaceae (1)
- Acidothermus (1)
- Adana Basin (1)
- Adana Becken (1)
- Aeromagnetik (1)
- African climate (1)
- Afrikanisches Klima (1)
- AgI (1)
- Air-pollution (1)
- Akkumulationsraten (1)
- Alaunschiefer (1)
- Algorithm (1)
- Alkenone (1)
- AlpArray (1)
- Alpine Fault (1)
- Alterationsgeochemie (1)
- Altersdatierung mit kosmogenen Nukliden (1)
- Altersmodelierung (1)
- Altiplano (1)
- Altlasten (1)
- Alum shale (1)
- Amery Oasis (1)
- Amery-Oase (1)
- Amplifier Lakes (1)
- Analogmodell (1)
- Analogue Model (1)
- Analyse komponentenspezifischer Kohlenstoffisotope (1)
- Anatolia (1)
- Anatolien (1)
- Anden / Störung <Geologie> / Strukturgeologie / Magnetotellurik / Chile <Nord> (1)
- Andenplateau Puna (1)
- Andes Centrales (1)
- Angewandte Geophysik (1)
- Anisotrope Inversion (1)
- Anisotropie der Leitfähigkeit (1)
- Antarctic ice (1)
- Antarctica (1)
- Anthropogenic sources (1)
- Antwortspektren (1)
- Apatit-(U-Th)/He Datierung (1)
- Apatit-Spaltspurendatierung (1)
- Apatite (U-TH)/HE (1)
- Apatite (U-Th)/He, apatite fission track dating (1)
- Applied Geophysics (1)
- Ar-Ar geochronology (1)
- Arabian Plate (1)
- Arabische Platte (1)
- Aralsee (1)
- Archaeolithoporella (1)
- Archetyp (1)
- Archäomagnetismus (1)
- Arctic Ocean (1)
- Arctic Siberia (1)
- Arctic lakes (1)
- Arctic nearhore zone (1)
- Arctic ocean (1)
- Arctic tundra ecosystems (1)
- Argentine margine (1)
- Arktik (1)
- Array Seismologie (1)
- Array-Entwurf (1)
- Artem Erkomaishvili (1)
- Asia (1)
- Asian Summer Monsoon (1)
- Asian monsoon (1)
- Asiatischer Sommermonsun (1)
- Asien (1)
- Asthenosphäre (1)
- Attribut-Analysen (1)
- Attributanalyse (1)
- Attribute (1)
- Auenbereich (1)
- Aufenthaltsdauer (1)
- Aufschluss-Modellierung (1)
- Auftretensrate (1)
- August 2002 flood (1)
- Auslösemechanismus (1)
- Australia (1)
- Australien (1)
- BRDF (1)
- Bachstufen (1)
- Baikalsee (1)
- Baladeh (1)
- Baldeggersee (1)
- Band (1)
- Barents Sea (1)
- Baryt (1)
- Basalt-Vulkane (1)
- Bay of Bengal (1)
- Bayes (1)
- Bayes'sche Netze (1)
- Bayesian classification (1)
- Bayesian networks (1)
- Bayesianism (1)
- Bayesische Statistik (1)
- Beamforming (1)
- Beckenentwicklung (1)
- Beckenstruktur (1)
- Beobachtung von Erdbebenquellen (1)
- Bergsturz (1)
- Bergstürze (1)
- Beton (1)
- Beweidung (1)
- Big Naryn complex (1)
- Bildbearbeitung (1)
- Biodiversität (1)
- Biogeochemie (1)
- Biogeochemistry (1)
- Biogeowissenschaften (1)
- Blattverschiebung (1)
- Blattwachse (1)
- Blei (1)
- Blockgletscher (1)
- Bodenbewegung (1)
- Bodenbewegungsmodellierung (1)
- Bodenfeuchtigkeit (1)
- Bodenheterogenität (1)
- Bodenkohlenstoff (1)
- Bodenparameter (1)
- Bodenwasser (1)
- Bodenwassergehalt (1)
- Bohrlochmessungen (1)
- Bohrlochrandausbrüche (1)
- Bolivian tin belt (1)
- Bor (1)
- Bor-isotopen (1)
- Borisotope; Zentrale Anden; kontinentaler Arc-Vulkanismus; Across-arc Variation; Borisotopenfraktionierung; krustale Kontamination (1)
- Boron isotopes (1)
- Boron isotopes; Central Andes; continental arc volcanism; across-arc variation; boron isotope fractionation; crustal contamination (1)
- Boundary element method (1)
- Brandenburg (1)
- Braunsbach Sturzflut (1)
- Braunsbach flash flood (1)
- Bruchflaechenstruktur (1)
- Bruchmechanik (1)
- Bruchmodel (1)
- Bruchverfolgung (1)
- Bruchzähigkeit (1)
- Bucht von Bengalen (1)
- Buntsandstein (1)
- CDOM (1)
- CMIP5 models (1)
- CRS (1)
- CU (1)
- Caimancito oil field (1)
- Caimancito-Ölfeld (1)
- Calderas (1)
- Campo petrolero Caimancito (1)
- Canada (1)
- Carbo-Iron® (1)
- Carbonate-Silicate reactions (1)
- Carbonates (1)
- Carrara marble (1)
- Carrara-marmor (1)
- Causal structure (1)
- Cenozoic aridification (1)
- Cenral Andes (1)
- Central Europe (1)
- Central Mediterranean (1)
- Central andes (1)
- Central-Asia (1)
- Cerrado (1)
- Chaco-Paraná Becken (1)
- Chaco-Paraná basin (1)
- Changing World (1)
- Channel Transmission Losses (1)
- Charnockit (1)
- Chile Rücken (1)
- Chile ridge (1)
- Chilean Andes (1)
- China (1)
- Chirete (1)
- Cimmerian orogeny (1)
- Cinética de fases (1)
- Cinética del querógeno (1)
- Climate Adaptation (1)
- Climate Mitigation (1)
- Climate reconstruction (1)
- Code_Aster (1)
- Colorado (1)
- Common-Reflection-Surface (1)
- Compound dislocation models (CDMs) (1)
- Computational Fluid Dynamics (CFD) (1)
- Congo Air Boundary (1)
- Connectivity (1)
- Contamination Control (1)
- Continental Rifts (1)
- Copernicus DEM (1)
- Core-mantle baundary (1)
- Cosmogenic Nuclides (1)
- Coulomb stress (1)
- Coulombspannung (1)
- Cretaceous (1)
- Cretaceous basin (1)
- Crustal density (1)
- Cuenca Cretácica (1)
- Cuenca intramontana (1)
- Cyclostratigraphy (1)
- Cyprus arc (1)
- D” Schicht (1)
- D” layer (1)
- DANSER (1)
- DAS (1)
- DEM noise (1)
- DNA preservation (1)
- Dabie Shan (1)
- Data-Mining (1)
- Datenanalyse (1)
- Datenbearbeitung (1)
- Datenfilter (1)
- Dauer der Bodenbewegung (1)
- Dauerfrostboden (1)
- Deep Learning (1)
- Deformación cuaternaria (1)
- Deformationsquellenmodellierung (1)
- Dehnungsdeformation (1)
- Dendrobaena veneta (1)
- Dendroklimatologie (1)
- Denitrifikation (1)
- Density modelling (1)
- Denudationsraten (1)
- Deuterium Exzesses (1)
- Deutschland (1)
- Diagenese (1)
- Diagenesis (1)
- Diaguita (1)
- Diamantstempelzelle (1)
- Diamantstempelzellen (1)
- Diatoms (1)
- Dichteheterogenitäten im oberen Mantel (1)
- Digital Elevation Model (1)
- Digital Elevation Models (1)
- Digitale Gesteinsphysik (1)
- Dike (1)
- Dinoflagellatenzyste (1)
- Discrete Element Method (1)
- Diskrete-Elemente-Methode (1)
- Dispersionskurven (1)
- Distally steepened ramps (1)
- Distribution functions with upper bound (1)
- Drohnen-Fernerkundung (1)
- Druck-Temperatur Bedingungen (1)
- Drucklösungsprozesse (1)
- Dryland Rivers (1)
- Dyke (1)
- Dämpfungstomographie (1)
- ENSO (1)
- ERA5 (1)
- EROEI (1)
- ETAS (1)
- ETAS Modell (1)
- ETAS model (1)
- EXAFS (1)
- Early Earth (1)
- Earth's mantle (1)
- Earthquake forecasting (1)
- Earthquake magnitude (1)
- Earthquakes (1)
- East African Plateau (1)
- Eastern Karoo Basin (1)
- Echtzeitanwendung (1)
- Edelgase (1)
- Edelgasisotope (1)
- Eifel (1)
- Eifel Depression (1)
- Eifeler Nord-Süd-Zone (1)
- Einengungsraten (1)
- Einsatzzeiten (1)
- Einzugsgebiet (1)
- Einzugsgebietshydrologie (1)
- Einzugsgebietsklassifizierung (1)
- Eisdamm (1)
- Eisdynamik (1)
- Eisenbahninfrastruktur (1)
- Eisenia fetida (1)
- Eismodell (1)
- Eklogite (1)
- Elastische Gesteinseigenschaften (1)
- Elastizitätsmodul (1)
- Elbe estuary (1)
- Elbe Ästuar (1)
- Electrical Resistivity Tomography (ERT) (1)
- Electrical resistivity tomography (1)
- Elektrische Widerstandstomographie (ERT) (1)
- EnGeoMAP 2.0 (1)
- EnMAP Satellit (1)
- EnMAP satellite (1)
- Endlagerung nuklearer Abfälle (1)
- Enhanced Geothermal Systems (1)
- Ensemble analysis (1)
- Ensemble-Analyse (1)
- Entwicklungsländer (1)
- Environmental sciences (1)
- Eocene (1)
- Eozän (1)
- Epithermal Ag-Sn deposits (1)
- Equatorial Pacific (1)
- Equatorial plasma irregularities (1)
- Erbeben (1)
- Erdbeben Modellierung (1)
- Erdbeben-Magnitude (1)
- Erdbebengefährdung (1)
- Erdbebengefährdungsabschätzungen (1)
- Erdbebeninteraktion (1)
- Erdbebenkatalogdaten (1)
- Erdbebenmodelierung (1)
- Erdbebenquellen-Array (1)
- Erdbebenquellinversion (1)
- Erdbebenschwarm 2008 (1)
- Erdbebenschäden (1)
- Erdbebenwechselwirkung (1)
- Erdbeeben (1)
- Erdbeobachtung (1)
- Erdfälle (1)
- Erdrutsche (1)
- Ereignissynchronisation (1)
- Error (1)
- Erz (1)
- Erzgebirge (1)
- Etendeka (1)
- Etna (1)
- Eulerian grid (1)
- Eulerische Gitter (1)
- Eurasian active margin (1)
- Eurasischer aktiver Kontinentalrand (1)
- Europe (1)
- European Alps (1)
- European basin system (1)
- Europäische Alpen (1)
- Event Koinzidenz Analyse (1)
- Exhumationsprozesse (1)
- Exhumationsraten (1)
- Exhumierung (1)
- Expositionsaltersdatierung (1)
- Expositionsmodellen (1)
- Expression (1)
- Extension (1)
- Extraction (1)
- Extremereignisse (1)
- Extremniederschlag (1)
- Extremniederschläge (1)
- Falten (1)
- FastScape (1)
- Fault Healing (1)
- Fault architecture (1)
- Fault interaction (1)
- Fe-Mg-carpholite (1)
- Fehlerquellen der Modellierung (1)
- Feinsedimente (1)
- Feld (1)
- Feldarbeit (1)
- Feldspat (1)
- Felsmechanik (1)
- Fen complex (1)
- Fernerkundung an Vulkanen (1)
- Ferroperiklas (1)
- Festigkeit (1)
- Festigkeit des Schiefer (1)
- Finnmark Platform (1)
- Firmicutes (1)
- Fission-track thermochronology (1)
- Flache Subduktion (1)
- Flachwassercarbonate (1)
- Flat subduction (1)
- Flood Forecasting (1)
- Flood frequency analysis (1)
- Flood regionalisation (1)
- Floods Directive (1)
- Fluid Flow (1)
- Fluid inclusions (1)
- Fluid-Gesteins-Wechselwirkung (1)
- Fluid-Gesteinswechselwirkungen (1)
- Fluid-Schmelze Wechselwirkung (1)
- Fluid-strömungen (1)
- Fluide (1)
- Fluidströmung (1)
- Fluoreszenzbildgebung (1)
- Flussbettmorphologie (1)
- Flussprozesse (1)
- Flussterrassen (1)
- Flutbasalt (1)
- Flüsse (1)
- Flüssigkeitseinschlüsse (1)
- Flüssigkeitsinklusionen (1)
- Folgenabschätzung (1)
- Foraminifera (1)
- Fore-Arc (1)
- Forecasting Framework (1)
- Foreland (1)
- Foreland basin (1)
- Foreland basins (1)
- Formación Yacoraite (1)
- Formationsschaden (1)
- Forschungsmethodik (1)
- Forstwirtschaft (1)
- Fotogrammetrie (1)
- Fourier analysis (1)
- Fourier spectra (1)
- Fourier-Spektren (1)
- Fracture mechanics (1)
- Freeze-Thaw-Cycles (1)
- Frost-Tau-Wechsel (1)
- Frühdiagenese (1)
- Frühe Erdgeschichte (1)
- Fundament (1)
- GDGT (1)
- GEDI (1)
- GLDAS (1)
- GMPE adjustment (1)
- GNSS-integrated water vapour (1)
- GRACE (1)
- Gabbro-Eklogit (1)
- Gangschwarm (1)
- Gasgeochemie (1)
- Gaylussite (1)
- Gebietszustand (1)
- Gebirgsbildung (1)
- Gebirgsbäche (1)
- Gebirgshydrologie (1)
- Gebäudenergiebedarf (1)
- Gefahren (1)
- Gefahrenanalyse (1)
- Gemmatimonadetes (1)
- Geochronology (1)
- Geodynamic Modeling (1)
- Geodynamic Modelling (1)
- Geodynamiche Modellierung (1)
- Geodynamics (1)
- Geodynamische Modellierung (1)
- Geodäsie (1)
- Geology (1)
- Geomagnetic activity (1)
- Geomagnetic index (1)
- Geomagnetic observatory (1)
- Geomagnetische Aktivität (1)
- Geomagnetischer Index (1)
- Geomagnetisches Observatorium (1)
- Geomechanical Model (1)
- Geomechanical Modelling (1)
- Geomechanik (1)
- Geomechanische Modellierung (1)
- Geomicrobiology (1)
- Geomikrobiologie (1)
- Geomorphology (1)
- Geophysics (1)
- Georgia (1)
- Georgian chant (1)
- Georgien (1)
- Georgische liturgische Gesänge (1)
- Geosciences (1)
- Geothermal monitoring (1)
- Geothermisches Monitoring (1)
- Geowissenschaften (1)
- Gerinne-Hang-Kopplung (1)
- Gerinnemorphologie (1)
- Geschiebetransport (1)
- Geschwindigkeitsmodell (1)
- Gestein-Wasser-Wechselwirkung (1)
- Gesteinsmagnetik (1)
- Glacial refugia (1)
- Glacier Mass Balances (1)
- Glaciers (1)
- Glasstruktur (1)
- Glazialisostasie (1)
- Gletschervorfeld (1)
- Global Navigation Satellite System (GNSS) (1)
- Global change (1)
- Global earthquake data (1)
- Global inversion (1)
- Globale Erdbebenkatalogdaten (1)
- Globale Inversion (1)
- Gläser (1)
- Gondwana (1)
- Grabenbruch (1)
- Grabenbrüche (1)
- Gravel-bed (1)
- Gravimetrie (1)
- Greenland ice cores (1)
- Ground Motion Prediction Equation (GMPE) (1)
- Groundwater (1)
- Grundgestein (1)
- Grundgesteinshöhe (1)
- Grundwasser (1)
- Grundwasserentwicklung (1)
- Grundwasserneubildung (1)
- Grundwassersanierung (1)
- Gulf of Mexico (1)
- H/V (1)
- HDAC (1)
- HP-HT Experimente (1)
- HP-HT experiments (1)
- HP/LT metamorphism (1)
- HP/LT-Metamorphose (1)
- Halobacteria (1)
- Halophile (1)
- Hangerosion (1)
- Hanghydrologie (1)
- Hangrutsch (1)
- Hauptspannungsachse (1)
- Haushalte (1)
- Hawaii (1)
- Hebung (1)
- Hebung des Plateaus (1)
- Hebungsgeschichte (1)
- Hebungsraten (1)
- Hercynian orogeny (1)
- Herdmechanismen (1)
- Herdzeit Parameter Abschätzung (1)
- Heterogenität (1)
- Heterozoan (1)
- Heterozoikum (1)
- Hidden Markov Model (HMM) (1)
- High-pressure/low-temperature rocks (1)
- Himalaja (Kaghan) (1)
- Himalaya (Kaghan Valley) (1)
- Himalaya-Tibet Orogen (1)
- Himalaya-Tibet orogen (1)
- Himalayas (1)
- Hitze (1)
- Hochdruck/Niedrigtemperatur Gesteine (1)
- Hochdruckrelikte (1)
- Hochdurchsatzsequenzierung (1)
- Hochland von Tibet (1)
- Hochplateau (1)
- Hochtemperatur Gesteinsdeformtion (1)
- Hochwasserregionalisierung (1)
- Hochwasserrekonstruktion (1)
- Hochwasserrisiko (1)
- Hochwasserrisikoanalysen (1)
- Hochwasserrisikokette (1)
- Hochwasserstatistik (1)
- Hochwassertypen (1)
- Hochwasservorhersage (1)
- Hohlzylinderversuche (1)
- Holzkompost (1)
- Home (1)
- Horizontal flux (1)
- Hotspot (1)
- HySpex (1)
- Hydratbildung (1)
- Hydrathabitus (1)
- Hydrogenase (1)
- Hydrogeophysics (1)
- Hydrogeopyhsik (1)
- Hydrogravimetrie (1)
- Hydrological Modelling (1)
- Hydrological extremes (1)
- Hydrus-2D (1)
- Hyperion (1)
- Hämmerlein (1)
- ICESat-2 (1)
- IHPV (1)
- IMPRESSIONS (1)
- Ice model (1)
- Iceland (1)
- Imaging spectroscopy (1)
- Impakt (1)
- In-Situ-Analyse (1)
- InSAR Datenanalyse (1)
- InSAR- Techniken (1)
- India (1)
- Indian Monsoon (1)
- Indian Monsoon Circulation (1)
- Indian Ocean (1)
- Indian Summer Monsoon (1)
- Indian summer monsoon (1)
- Indische Monsunzirkulation (1)
- Indische Sommer Monsun (1)
- Indischer Sommermonsun (1)
- Indonesien (1)
- Induzierte Seismizität (1)
- Injektion (1)
- Injektionsschema (1)
- Interaktion zwischen sich ausbreitenden Riftsegmenten (1)
- Interferometrie (1)
- Interseismic strain rates (1)
- Interseismiche Dehnungsraten (1)
- Intramontane basin (1)
- Intramontanes Becken (1)
- Inverse modelling (1)
- Inversions-Theorie (1)
- Inversionstheorie (1)
- Ion-Beam (FIB) (1)
- Ionic liquids (1)
- Ionosphäre (1)
- Island (1)
- Isotope (1)
- Isotopen (1)
- Isotopenfraktionierung (1)
- Isotopes (1)
- Isábena Einzugsgebiet (1)
- Isábena catchment (1)
- Isótopos de Boro (1)
- Jaguaribe Basin (1)
- June 2013 flood (1)
- Kanada (1)
- Karakoram (1)
- Karakorum (1)
- Karbonat-Silikat-Reaktionen (1)
- Karbonat-Stabilität (1)
- Karbonatplattformen (1)
- Karbonatrampen (1)
- Karbonatschmelze (1)
- Karpholithe (1)
- Karst (1)
- Kausalstruktur (1)
- Kenia (1)
- Kenya (1)
- Kerguelen (1)
- Kerogenkinetik (1)
- Klimaanpassung (1)
- Klimaschutz (1)
- Klimatologie (1)
- Klimavariabilität (1)
- Klimaveränderung (1)
- Klimaänderungen (1)
- Knickpoint (1)
- Knickpoint retreat (1)
- Knickpunkt (1)
- Knickpunkt-Rückzug (1)
- Kohlendioxid (1)
- Kohlengrubenabraum (1)
- Kohlenstoff-Budget (1)
- Kohlenstoffdioxid (1)
- Kohlenstoffisotope (1)
- Kohlenstoffkreislauf (1)
- Kohlenstoffspeicher (1)
- Kolloidtransport (1)
- Kongo Luftmassengrenze (1)
- Konin region (1)
- Kontaminationskontrolle (1)
- Kontinentale Kollision (1)
- Kontinentalrand (1)
- Koppelung (1)
- Korallen (1)
- Korrelation (1)
- Kreide (1)
- Kreidebecken (1)
- Kriecheigenschaften (1)
- Kruste (1)
- Krustenstruktur der Süd-Türkei (1)
- Krustenstruktur des Eratosthenes Seeberges (1)
- Krustenverformungen (1)
- Kugelflächenfunktionen (1)
- Kuilyu complex (1)
- Kultivierung (1)
- Kumamoto Erdbeben (1)
- Kumamoto earthquake (1)
- Kupfer (1)
- Kwajalein (1)
- Känozoische Aridifizierung (1)
- Küste (1)
- Küstenlinien (1)
- L-Asterisk (1)
- LA-ICP-MS (1)
- Lake Baikal (1)
- Lake Challa (1)
- Lake Mead (1)
- Lake Naivasha (1)
- Lake Towuti (1)
- Land use change (1)
- Landformen (1)
- Landnutzungsänderung (1)
- Landsat (1)
- Landsat. (1)
- Landscape Evolution (1)
- Landscape Response (1)
- Landschaftseffekte (1)
- Landschaftspräferenzen (1)
- Landslide inventory (1)
- Landslide susceptibility (1)
- Landwirtschaft (1)
- Laptev Sea region (1)
- Larix larch (1)
- Laser ablation (1)
- Laserheizsystem (1)
- Last Glacial (1)
- Late Quaternary (1)
- Lateglacial (1)
- Laufzeitresiduen (1)
- Lava dome (1)
- Lavadom (1)
- Lavafontänen (1)
- Lawinen (1)
- Lena Delta (1)
- Lena delta (1)
- Letztes Glazial (1)
- Lichenometrie (1)
- Liguride Complex (1)
- Limnologie (1)
- Liquiñe-Ofqui Störungszone (1)
- Liquiñe-Ofqui fault zone (1)
- Lithium (1)
- Lithospheric Deformation (1)
- Lithospheric strength (1)
- Lithospheric structure (1)
- Lithosphärenfestigkeit (1)
- Lithosphärische Deformation (1)
- Llaima Vulkan (1)
- Llaima volcano (1)
- Lokalisierte Deformation (1)
- Lokalisierung von Deformation (1)
- Lokalisierung von Verformung (1)
- Lonar lake (1)
- Lonarsee (1)
- Long-Term (1)
- Loppa High (1)
- Lower Devonian (1)
- Lumineszenz (1)
- Lusatia (1)
- Luxembourg (1)
- Luxemburg (1)
- Lycian Nappes (1)
- Lykischen Decken (1)
- Lysimeter (1)
- MC-ICP-MS (1)
- MO (1)
- MSPAC (1)
- Mackenzie Delta (1)
- Mackenzie-Delta (1)
- Magma-Entgasung (1)
- Magmagänge (1)
- Magmatismus (1)
- Magnesit (1)
- Magnetostratigraphie (1)
- Magnetotelluric (1)
- Magnetotellurics (1)
- Mahalanobis distance (1)
- Mahalanobis-Distanz (1)
- Malta (1)
- Mantel (1)
- Mantel Plume (1)
- Mantelplumes (1)
- Mantle (1)
- Mantle Plume (1)
- Mantleplumes (1)
- Marmarameer (1)
- Martinez del Tineo (1)
- Massenaussterben (1)
- Massenversatzprozesse (1)
- Mediterranes Tiefdrucksystem (1)
- Meditteranean sea (1)
- Meeressedimente (1)
- Melilitit (1)
- Melt inclusions (1)
- Merapi (1)
- Mesozoic (1)
- Mesozoikum (1)
- Metamorphism (1)
- Metamorphose (1)
- Metasomatism (1)
- Metasomatose (1)
- Methan (1)
- Methodology (1)
- Mexico (1)
- Mexiko (1)
- Middle East (1)
- Middle Eocene deformation (1)
- Middle Strand (1)
- Mikro-CT (1)
- Mikrobieller Abbau von organischen Material (1)
- Mikroplatte (1)
- Mikrostruktur (1)
- Mikrostrukturelle (1)
- Mikrostrukturen (1)
- Mikrozonierung (1)
- Mineralogie (1)
- Mineralreaktion (1)
- Mineralverwitterungsreaktionen (1)
- Mineralzusammensetzung (1)
- Mittelmeer (1)
- Mittelmeerraum (1)
- Mixmodelle (1)
- Mobile Belts (1)
- Model (1)
- Modell (1)
- Modellanpassung (1)
- Modellierung der Wassertrübung (1)
- Modellierung des seismischen Zyklus (1)
- Molybdän (1)
- Moment tensor inversion (1)
- Momententensorinversion (1)
- Monazit (1)
- Mondsee (1)
- Mongolei (1)
- Mongolia (1)
- Morphometrie (1)
- Morphometry (1)
- Multi-Hazard (1)
- Multiproxy-Untersuchung (1)
- Multiskalen Netzwerk (1)
- Multivariate Analyse (1)
- Multivariate statistic (1)
- Muscovit (1)
- Muster der Bodenfeuchte (1)
- Mustererkennung (1)
- NE Pamir (1)
- NEG (1)
- NO2 (1)
- NW Argentina (1)
- NW Himalaja (1)
- NW Himalaya (1)
- NW Turkey (1)
- Naher Osten (1)
- Naivasha See (1)
- Namche Barwa (1)
- Namibia (1)
- NatRiskChange (1)
- Naturrisiken (1)
- Natürliche Staudämme (1)
- Near-surface geophysics (1)
- Nearshore zone (1)
- Neotectonics (1)
- Nettorotation der Lithosphäre (1)
- Neutronen (1)
- Nevado Coropuna (1)
- Nicht-Einmaligkeit (1)
- Niederschlag (1)
- Niedrigwasser (1)
- Niger (1)
- Niger River (1)
- Non-uniqueness (1)
- Nordanatolische Störungszone (1)
- Nordeste (1)
- Nordostdeutsches Becken (1)
- Nordostdeutsches Tiefland (1)
- North Anatolian Fault (1)
- North Anatolian Fault Zone (1)
- North Calabrian Unit (1)
- North-East German Plain (1)
- Northeast German Basin (1)
- Northern Sierras Pampeanas (1)
- Northwestern Anatolia (1)
- Nuklide (1)
- Numerische 2D Modellierung (1)
- Nährstoffe (1)
- Nährstoffeinträge (1)
- Nährstoffretention (1)
- ODP Leg 194 (1)
- OSL (1)
- Oberfläche (1)
- Oberflächenexpositionsdatierung (1)
- Oberflächennahe Geophysik (1)
- Oberflächenwärmefluss (1)
- Oberflächenwärmefluß (1)
- Ocean Colour satellite data (1)
- Ocean color remote sensing (1)
- Ocean sciences (1)
- Oligo-Miocene (1)
- Oligozän-Miozän-Grenze (1)
- OpenForecast (1)
- OpenStreetMap (1)
- Optical remote sensing (1)
- Optical sensor (1)
- Optische Sensoren (1)
- Organic matter mineralization (1)
- Organofazies (1)
- Ortscharakterisierung (1)
- Ortseffekte (1)
- Ostafrika (1)
- Ostafrikanisches Rift (1)
- Ostafrikanisches Riftsystem (1)
- Ostafrikansches Rift (1)
- Ostkordillere (1)
- PLA (1)
- PM10, PM2, PM1 (1)
- PPGIS (1)
- Palaeoecology (1)
- Palaeoklima (1)
- Paleoclimate (1)
- Paleoclimate dynamics (1)
- Paleofloods (1)
- Paleogeography (1)
- Paleolimnology (1)
- Paleomagnetism (1)
- Paleomagnetismus (1)
- Paläo-See Mweru (1)
- Paläo-Strain-Berechnung (1)
- Paläoaltimetrie (1)
- Paläohochwasser (1)
- Paläohydrologie (1)
- Paläointensität (1)
- Paläoklimadynamik (1)
- Paläomagnetismus (1)
- Paläosekularvariation (1)
- Paläotektonik (1)
- Paläotopographie (1)
- Pamir-Tien Shan (1)
- Panasqueira (1)
- Parallel Seismik (1)
- Paris Basin (1)
- Pariser Becken (1)
- Particle swarm optimization (1)
- Partikel Swarm Optimierung (1)
- Partikelschwarm-Optimierung (1)
- Passive Kontinentalränder (1)
- Passive margins (1)
- Patagonien (1)
- Patagonien ; Neogen ; Hebung ; Subduktion ; Anden (1)
- Pattern Recognition (1)
- Patterns (1)
- Periglazial (1)
- Periglazialgeomorphologie (1)
- Permafrost-Taustörungen (1)
- Permafrostdegradation (1)
- Permafrostlandschaften (1)
- Permafrostsedimente (1)
- Permeabilität (1)
- Permeabilitätsentwicklung (1)
- Petrology (1)
- Pfadanalysen (1)
- Pfahl (1)
- Pflanzen-Habitat Interaktionen (1)
- Pflanzenwachs (1)
- Pflanzenwachstum (1)
- Pflanzenwasserzustand (1)
- Pflaume (1)
- PhaseKinetics (1)
- PhasePaPy (1)
- Phasenkinetik (1)
- Phasenpicker (1)
- Photozoan (1)
- Photozoikum (1)
- Phytoplankton (1)
- Piano delle Concazze (1)
- Picker (1)
- Pinus pinaster (1)
- Plattenbewegungen (1)
- Plattentektonik (1)
- Playa (1)
- Plume-Rücken Interaktion (1)
- Poland (1)
- Polarimetrie (1)
- Polarimetry (1)
- Polen (1)
- Pollenanalyse (1)
- Pollenproduktivitätsschätzungen (1)
- Polynia (1)
- Pontiden (1)
- Pontides (1)
- Porentypen in Karbonate (1)
- Porphyrische Kupferlagerstätte (1)
- Posidonia shale (1)
- Posidonienschiefer (1)
- Potsdam (1)
- Precipitation (1)
- Probabilistic regional envelope curves (1)
- Probabilistische Regionale Hüllkurven (1)
- Probenahmestrategie (1)
- Procrustes rotation analysis (1)
- Prokrustes Analyse (1)
- Prozessidentifikation (1)
- Präzision Gartenbau (1)
- Prüfköpfe (1)
- Psychologie (1)
- Pull-Apart (1)
- Puna Plateau (1)
- Puna plateau (1)
- Qilian mountains (1)
- Quantitative Daten (1)
- Quartäre Deformation (1)
- Quaternary (1)
- Quaternary deformation (1)
- Quell-Array optimales Design (1)
- Quellarray (1)
- Quelle Inversion (1)
- Quellenparameter (1)
- Quellenumkehr (1)
- Quercus ilex (1)
- Quercus pubescens (1)
- RCP scenarios (1)
- REVEALS (1)
- Radar-Satelliteninterferometrie (1)
- Radiokarbondatierung (1)
- Raman-Spektroskopie (1)
- Ramos X-11 (1)
- Rauheit (1)
- Raumwellen (1)
- Reaktionspfadmodellierung (1)
- Reaktivierung von Störungszonen (1)
- Receiver Function (1)
- Receiver Functions (1)
- Receiver Funktionen (1)
- Recurrence network (1)
- Recurrence plot (1)
- Reflectivity (1)
- Regensturm (1)
- Region Konin (1)
- Regional Climate Model (1)
- Regressionsanalyse (1)
- Regularisierung (1)
- Reibung an Plattengrenzen (1)
- Reifegradbezogene Biomarker (1)
- Remote Sensing (1)
- Reservoir Networks (1)
- Rhenohercynian Zone (1)
- Rhenohercynische Zone (1)
- Rheological modeling (1)
- Rheologische Modellierung (1)
- Rhizosphere (1)
- Riff (1)
- Ringstörungen (1)
- Risikoanalyse (1)
- Risikobewertung von Vulkanausbrüchen (1)
- Rissmechanik (1)
- Risstransmissivität (1)
- River (1)
- River Incision Model (1)
- Rupture Propagation (1)
- Russia (1)
- Russian Arctic (1)
- Réunion (1)
- Río Pescado (1)
- Röntgenabsorptionspektroskopie (1)
- Röntgenabsorptionsspektroskopie (1)
- Rückenkollision (1)
- Rückensubduktion (1)
- S Phase (1)
- S-Phase (1)
- SEC (1)
- SIMS (1)
- SIO₂ (1)
- SPAC (1)
- SRTM (1)
- Sachsengängerei (1)
- Sahel (1)
- Salt Range (1)
- Salt pan (1)
- Salta Rift (1)
- Salta basin (1)
- Salta-Becken (1)
- Salzgestein (1)
- Salzpfanne (1)
- Samara (1)
- San Andreas Fault (1)
- San Andreas Verwerfung (1)
- Sandstein (1)
- Santa Cruz formation (1)
- Santa-Barbara system (1)
- Saprolit (1)
- Sardinia (1)
- Sardinien (1)
- Satelliten-Fernerkundung (1)
- Satellitenbilder (1)
- Satellitenmission Swarm (1)
- Sauerstoff (1)
- Sauerstoffisotope (1)
- Savannen-Ökologie (1)
- Saxo-Thuringia (1)
- Scaling (1)
- Schaden (1)
- Schadensabschätzung (1)
- Schallemissionen (1)
- Scherzonen (1)
- Schmelzeinschlüsse (1)
- Schmelzstruktur (1)
- Schnee (1)
- Schwemmfächer (1)
- Schwerkraft (1)
- Sea of Marmara (1)
- SeaWiFS Ocean-Colour Satellitendaten (1)
- Sediment Fingerprinting (1)
- Sediment Flux (1)
- Sediment Transport (1)
- Sedimentationsdynamik (1)
- Sedimentbecken (1)
- Sedimente (1)
- Sedimentenabfolge (1)
- Sedimentfalle (1)
- Sedimentfazies (1)
- Sedimentfracht (1)
- Sedimentmächtigkeit (1)
- Sedimentquellenidentifizierung (1)
- Sedimenttransportsystem (1)
- Sedimentvolumen (1)
- Seeausbrüche (1)
- Seedurchmischung (1)
- Seespiegelschwankungen (1)
- Seestandsänderung (1)
- Seesystemreaktionen (1)
- Seewasserhaushalt (1)
- SeisComP3 (1)
- Seismic Array Methods (1)
- Seismic arrays (1)
- Seismik (1)
- Seismische Arrays (1)
- Seismische Geschwindigkeiten (1)
- Seismische Interferometrie (1)
- Seismische Tomographie (1)
- Seismizität und Tektonik (1)
- Seismizitätsmodellierung (1)
- Seltenerdelemente (1)
- Sentinel 2 (1)
- Sentinel-2 MSI (1)
- Shear Zone (1)
- Shortening (1)
- Shortening rates (1)
- Shyok Fluss (1)
- Shyok River (1)
- Siberian larch (1)
- Sibirien (1)
- Sibirien <Nord> (1)
- Sibirienhoch (1)
- Sichuan (1)
- Sierras Pampeanas (1)
- Signalbildung (1)
- Signalweiterleitung (1)
- Silikatschmelze (1)
- Silikatverwitterung (1)
- Sinkholes (1)
- Skala (1)
- Skalierung (1)
- Skarn (1)
- Slip Distribution (1)
- Slope (1)
- Sn (1)
- Software (1)
- Soil hydrology (1)
- Soil moisture (1)
- Solar irradiation (1)
- Solare Austrahlung (1)
- Solid Earth sciences (1)
- Sorption (1)
- South Chile (1)
- South Eifel (1)
- Southatlantic (1)
- Southeast Asia (1)
- Southern Apennines (1)
- Southern Kyrgyzstan (1)
- Soziale Medien (1)
- Space climate (1)
- Space weather (1)
- Spalt Spuren (1)
- Spalteneruption (1)
- Spannung (1)
- Spannungsfeld des späten Känozoikums (1)
- Spannungsmessung (1)
- Spannungsmuster (1)
- Spannungsänderungen (1)
- Spektralanalyse (1)
- Spiti valley (1)
- Spitsbergen (1)
- Spity Valley (1)
- Spitzbergen (1)
- Spread F (1)
- Spröde Vorläufer (1)
- Spurenelement-Partitionierung (1)
- Spurenelementverteilung (1)
- Spätglazial (1)
- Spätquartär (1)
- Sri Lanka (1)
- Stabile Isotope (1)
- Stabile Isotopen (1)
- Stabile Sauerstoff- und Kohlenstoffisotope (1)
- Stadtentwicklung (1)
- Stalagmiten (1)
- Standort des Streuers (1)
- Starkregen (1)
- Statistical seismology (1)
- Statistische Seismologie (1)
- Steilwinkel-Analyse von PcP (1)
- Stochastischer Algorithmus (1)
- Strahlung und chemische Eigenschaften (1)
- Strain Localisation (1)
- Strain Localization (1)
- Stratigrafie (1)
- Stratigraphie (1)
- Stream Power Law (1)
- Stressmodellierung (1)
- Strike-Slip Störungen (1)
- Strike-slip fault (1)
- Stromsektor (1)
- Structure-from-motion (1)
- Strukturmodellierung (1)
- Sturzflut (1)
- Sturzfluten (1)
- Städe (1)
- Städte Effizienz (1)
- Störungen (1)
- Störungsbau (1)
- Störungsinteraktion (1)
- Störungszonen (1)
- Störungszonenarchitektur (1)
- Subduktionsbeben (1)
- Subsidenzgeschichte (1)
- Subsurface Biosphere (1)
- Suguta Tal (1)
- Suguta Valley (1)
- Suigetsu (1)
- Sulfatreduktion (1)
- Sumatra (1)
- Sumatra Störung (1)
- Sumatra fault (1)
- Superconducting gravimetry (1)
- Supraleit-Gravimetrie (1)
- Supraleitender Gravimeter (SG) (1)
- Suspendsionsfracht (1)
- Swarm constellation (1)
- Sweet (1)
- Synchronisation von Ereignissen (1)
- Syntaxe (1)
- Synthetic Aperture Radar (1)
- Synthetische Sandsteine (1)
- Süd Chile (1)
- Süd-Türkei (1)
- Südatlantik (1)
- Südeifel (1)
- Südostasien (1)
- TDR (1)
- TIME-GCM (1)
- TRMM (1)
- Taifune (1)
- TanDEM-X (1)
- Tarim Basin (1)
- Tarutung (1)
- Tasas de acortamiento (1)
- Taylor’s law (1)
- Tectona grandis (1)
- Tectonic Evolution (1)
- Tectonic geomorphology (1)
- Tektonische Geomorphologie (1)
- Temperatur (1)
- Temperaturfeld (1)
- Tendürek Vulkan (1)
- Tendürek volcano (1)
- Teteriv (1)
- Thermal (1)
- Thermal modeling (1)
- Thermal-conductivity (1)
- Thermisch (1)
- Thermische Modellierung (1)
- Thermokarstprozesse (1)
- Tian Shan (1)
- Tian-Shan (1)
- Tianshan orogenic belt (1)
- Tibet (1)
- Tiefbeben und Kernexplosionen (1)
- Tiefendeformation (1)
- Tiefenversickerung (1)
- Tiefer See (1)
- Tien-Shan (1)
- Tiltmeter (1)
- Time series analysis (1)
- Tomographie (1)
- Tomographie des elektrischen Widerstands (1)
- Tonian–Cryogenian (1)
- Tonmineralien (1)
- Topographie (1)
- Torsion Experiments (1)
- Torsionsexperimente (1)
- Tote Meer (1)
- Totes Meer (1)
- Transferverluste in Flüssen (1)
- Transformation (1)
- Transformation hydrologischer Signale (1)
- Transformstörung (1)
- Transnationalismus (1)
- Treibhausgase (1)
- Trendanalysen (1)
- Triangular dislocations (TDs) (1)
- Trier-Luxembourg Basin (1)
- Trier-Luxembourg Embayment (1)
- Trier-Luxemburger Becken (1)
- Trier-Luxemburger Bucht (1)
- Tritium Assay (1)
- Tritium Versuchsanordnung (1)
- Trockenflüsse (1)
- Tropospheric nitrogen-dioxide (1)
- Tsunami-Frühwarnsystem (1)
- Tsunami-Risiko (1)
- Turbidite (1)
- Turbidites (1)
- Turbidity retrieval (1)
- Turmalin (1)
- Twitter (1)
- U-Pb Geochronologie (1)
- U-Pb geochronology (1)
- UHI (1)
- UHP (1)
- UV fs laser ablation (1)
- UV-Lasermikrodissektion (1)
- UV-laser microdissection (1)
- Ukraine (1)
- Uk’37 (1)
- Ultra-Niedriggeschwindigkeitszonen (1)
- Ultraschall (1)
- Umweltmonitoring (1)
- Umweltrekonstruktion (1)
- Uncertainty Analysis (1)
- Uncertainty Processor (1)
- Unsupervised Learning (1)
- Unterdevon (1)
- Untergrund (1)
- Untergrunduntersuchung der Biosphäre (1)
- Unterrichtsmethoden (1)
- Untertage-Kohlevergasung (1)
- Unüberwachtes Lernen (1)
- Uplift Rates (1)
- Uran (1)
- Uran-Blei-Datierung (1)
- VI (1)
- VIIRS DNB (1)
- Validation (1)
- Vansee (1)
- Variabilität (1)
- Variabilität von Bodenbewegung (1)
- Variscan orogeny (1)
- Vegetationsbedeckung (1)
- Verarbeitung seismischer Daten (1)
- Verdichtung (1)
- Verformungslokalisierung (1)
- Verkürzung (1)
- Verschüttungsaltersdatierung (1)
- Verteilungsfunktionen mit einer oberen Grenze (1)
- Vertical flux (1)
- Vertreibung (1)
- Verwitterungsfeedback (1)
- Videoanalyse (1)
- Viskositätsstruktur im oberen Mantel (1)
- Volcano (1)
- Volcano deformation modelling (1)
- Vorelandbecken (1)
- Vorland (1)
- Vorlandbeckenentwicklung (1)
- Vorlanddeformation (1)
- Vs Profile (1)
- Vs profiles (1)
- Vulcano (1)
- Vulkan Verformung (1)
- Vulkaniklastika (1)
- Vulkanismus (1)
- Vulkanologie (1)
- Vulkanverformungsmodellierung (1)
- Vulkanüberwachung (1)
- WGHM (1)
- Waldbewirtschaftung (1)
- Waldumbau (1)
- Warve (1)
- Warves (1)
- Wasser-Gesteins-Wechselwirkungen (1)
- Wasser-Monitoring (1)
- Wasserdampf (1)
- Wassergütemodellierung (1)
- Wasserpflanzen (1)
- Wasserqualität (1)
- Wasserspeicheränderungen (1)
- Water Availability (1)
- Water resources (1)
- Wavelet (1)
- Weather (1)
- Weilerbach-Mulde (1)
- Well-log analysis (1)
- Wellenausbreitung (1)
- Wellenbrechung und Diffraktion (1)
- Wellengeschwindigkeit (1)
- Wellengeschwindigkeiten (1)
- Wellenleiter (1)
- Weltraumklima (1)
- Weltraumwetter (1)
- Wenchuan (1)
- West Fault Zone (1)
- West Turkey (1)
- West Türkei (1)
- Westböhmen (1)
- Western Bug (1)
- Western Interior Basin (1)
- Western Qaidam Basin (1)
- Wiederkehr (1)
- Windböen (1)
- Winddynamik (1)
- Winderosion (1)
- Wirtsgesteinsskala (1)
- Wittlicher Senke (1)
- Wofram-Zinn Lagerstätte (1)
- WorldDEM (1)
- WorldView-2 (1)
- Wuchiapingian (1)
- Wuchiapingium (1)
- Würzburg (1)
- X-ray absorption spectroscopy (1)
- XANES (1)
- XAS (1)
- XRF (1)
- Yacoraite Formation (1)
- Yamal (1)
- Yarlung-Tsangpo Gorge (1)
- Yarlung-Tsangpo Schlucht (1)
- Yatta (1)
- Young's modulus (1)
- Younger Dryas (1)
- Zeitanhängig (1)
- Zeitserie (1)
- Zeitskala (1)
- Zentral Asien (1)
- Zerstörungsfreie Prüfung (1)
- Zink (1)
- Zinn (1)
- Zipf’s law (1)
- Zusammengesetztes Dislokationsmodel (CDM) (1)
- Zustands-Übergangs-Modelle (1)
- Zyklostratigraphie (1)
- Zypernbogen (1)
- accumulation (1)
- accumulation rates (1)
- acidophilic microorganisms (1)
- acoustic emissions (1)
- activ continental margin (1)
- active faulting (1)
- active seismic (1)
- active source data (1)
- adapation (1)
- adaptation (1)
- adaption measure (1)
- aero (1)
- aftershock (1)
- aftershock sequence (1)
- aftershocks (1)
- age modeling (1)
- age-related biomarkers (1)
- airglow (1)
- aktive Quelldaten (1)
- aktive Seismik (1)
- aktive Verwerfungen (1)
- aktive Weitewinkel-Seismik (1)
- aktiver Kontinentalrand (1)
- alaskan tundra (1)
- alkenones (1)
- allochthon (1)
- alluvial (1)
- alluvial channel morphology (1)
- alpine (1)
- alpine catchments (1)
- alps (1)
- alteration geochemistry (1)
- ambient vibration (1)
- anaerobe Inkubationensexperimente (1)
- anaerobic incubation experiments (1)
- analysis of pathways (1)
- angewandte Geophysik (1)
- anisotropic inversion (1)
- annually laminated sediments (1)
- antecedent conditions (1)
- applied geophysics (1)
- aquatic ecosystems (1)
- aquatischen Ökosystemen (1)
- archeomagnetism (1)
- archetype (1)
- architecture (1)
- arctic water bodies (1)
- area (1)
- argentina (1)
- argon (1)
- arktische Gewässer (1)
- arktischer Nahküstenbereich (1)
- array design (1)
- artificial light (1)
- artificial mixtures (1)
- artificial neural networks (1)
- assimilation (1)
- asthenosphere (1)
- asthenospheric slab-window (1)
- asthenospherisches "slab-window" (1)
- astronomical calibration (1)
- asymmetric pair distribution function (1)
- attribute analysis (1)
- attributes (1)
- authigene Mineralbildung (1)
- authigenic mineral formation (1)
- autochthon (1)
- automatic classification (1)
- automatic processing (1)
- automatische Klassifizierung (1)
- b-Wert Kartierung (1)
- b-value map (1)
- barite (1)
- barrow (1)
- basaltic volcanoes (1)
- basement rock (1)
- basin evolution (1)
- basin structure (1)
- bat fatalities (1)
- beam forming (1)
- bedload transport (1)
- bedrock elevation (1)
- beginnende Kontinent-Kontinent Kollision (1)
- beobachtende Seismologie (1)
- biodegradación (1)
- biodegradation (1)
- biodiversity (1)
- biodiversity decline (1)
- bioenergy (1)
- biofuel (1)
- biogeoscience (1)
- biologischer Abbau (1)
- biomarcadores diagnósticos de edad (1)
- biomarcadores diagnósticos de madurez (1)
- biomaterials (1)
- blueSeis-3A sensors (1)
- body waves (1)
- bolivianischen Zinngürtels (1)
- boreal forests (1)
- borehole breakouts (1)
- borehole leakage (1)
- boron (1)
- bottom water (1)
- bottom waters (1)
- boundary element method (1)
- brittle deformation (1)
- brittle precursors (1)
- burial dating (1)
- calc-alkaline (1)
- calcium phosphate (1)
- calcium phosphate hybrid material (1)
- calibration (1)
- campo de esfuerzo del Cenozoico tardío (1)
- canopy height (1)
- carbon budget (1)
- carbon cycling (1)
- carbon dioxide exchange (1)
- carbon export (1)
- carbon isotopes (1)
- carbon-cycle (1)
- carbonate (1)
- carbonate melt (1)
- carbonate platforms (1)
- carbonate pore types (1)
- carbonate ramps (1)
- carbonate stability (1)
- carbonate systems (1)
- carbonates (1)
- carpholite (1)
- catchment (1)
- catchment classification (1)
- catchment hydrology (1)
- catchment state (1)
- catchments (1)
- cell counts (1)
- cellulose (1)
- cement (1)
- central Andes (1)
- central Mediterranean (1)
- central Poland (1)
- central south island (1)
- central-eastern Beringia (1)
- change detection (1)
- channel steps (1)
- channel-hillslope coupling (1)
- charnockite (1)
- chemical dating (1)
- chemical weathering (1)
- chemical-mechanical interaction (1)
- chemische Datierung (1)
- chemische Verwitterung (1)
- chilenische Anden (1)
- chitosan (1)
- chronology (AICC2012) (1)
- circular statistics (1)
- circulation (1)
- cirrus detection (1)
- cities (1)
- city clusters (1)
- city of Potsdam (1)
- city of Wuerzburg (1)
- clay mineral (1)
- clima (1)
- climate change adaptation (1)
- climate change impact (1)
- climate dynamics (1)
- climate extreme events (1)
- climate global and local patterns (1)
- climate impacts (1)
- climate networks (1)
- climate reconstruction (1)
- climatic change (1)
- climatolgoy (1)
- clinopyroxenite (1)
- closed chamber method (1)
- cloud detection (1)
- coal mine waste (1)
- coesite (1)
- coherency (1)
- coherent noise (1)
- collapse (1)
- colloid transport (1)
- combinatorial inverse modelling (1)
- complex network (1)
- complex networks (1)
- complex systems (1)
- complexes (1)
- composite properties (1)
- compound-specific stable carbon isotope analyses (1)
- compression (1)
- computational ethnomusicology (1)
- computational seismology (1)
- computergestützte Musikethnologie (1)
- computergestützte Seismologie (1)
- concrete (1)
- conductivity anisotropy (1)
- conflict (1)
- continental breakup (1)
- continental collision (1)
- continental collision zones (1)
- continental lithosphere (1)
- continental margins (1)
- controlled source wide angle seismic (1)
- controlo estrutural (1)
- convective available potential energy (1)
- convective available potential energy (CAPE) (1)
- convolutional neural network (1)
- copper (1)
- corals (1)
- core-mantle boundary (1)
- cosmic rays (1)
- cosmic-ray (1)
- cosmogenic (1)
- cosmogenic AL-26 (1)
- cosmogenic nuclide dating (1)
- cosmogenic radionuclide-based dating (1)
- cosmogenic radionuclides (1)
- counterclockwise block rotation between overlapping rift segments (1)
- coupled fluid and heat transport (1)
- coupling (1)
- crack (1)
- creep properties (1)
- critical meteorological condition (1)
- critical zone (1)
- crop modeling (1)
- crustal deformations (1)
- crustal stress (1)
- crustal structure of south central Turkey (1)
- crustal structure of the Eratosthenes Seamount (1)
- crystalline (1)
- cuenca intermontana (1)
- cultivation (1)
- d-excess (1)
- damage assessment (1)
- damage modelling (1)
- data analysis (1)
- data filtering (1)
- data fusion (1)
- data processing (1)
- data science (1)
- data-mining (1)
- decision tree (1)
- decision trees (1)
- deep carbon (1)
- deep crust (1)
- deep earthquakes and nuclear explosions (1)
- deep permafrost carbon (1)
- deep seated landslide (1)
- deep seepage (1)
- deforestation (1)
- deformation mechanisms (1)
- deformation monitoring (1)
- deformation source modeling (1)
- degradation (1)
- delta-c-13 (1)
- dendroclimatology (1)
- dendrometer measurements (1)
- denitrification (1)
- density modeling (1)
- density-driven flow (1)
- denudation (1)
- denudation processes (1)
- denudation rates (1)
- deposits (1)
- depósitos de volfrâmio-estanho (1)
- der Städtische Wärmeinseleffekt (1)
- der Urbane Hitzeinsel Effekt (1)
- der Urbane Hitzeinsel Effekt basierend auf Landoberflächentemperatur (1)
- detrital carbonate (1)
- developing countries (1)
- dew-point temperature (1)
- diagenesis (1)
- diagenetische Prozesse (1)
- diamond anvil cell (1)
- diamond anvil cells (1)
- diatoms (1)
- dichtegetriebene Strömung (1)
- die Stadtform (1)
- digital image analysis (1)
- digitale Bildanalyse (1)
- dike pathways (1)
- dip-coating (1)
- dispersion curves (1)
- dissolution (1)
- distal steil ansteigende Rampen (1)
- ditch irrigation (1)
- diversity (1)
- drained lake basins (1)
- dreieckige Dislokationen (TDs) (1)
- drought (1)
- duration (1)
- dust sources (1)
- dynamic topography (1)
- dynamische Topographie (1)
- décollement (1)
- early diagenesis (1)
- early earth tectonics (1)
- early eocene (1)
- early warning (1)
- earth mantle (1)
- earth system model (1)
- earth system models (1)
- earth's mantle (1)
- earthquake bulletin data (1)
- earthquake damage (1)
- earthquake forecasting (1)
- earthquake location (1)
- earthquake source array (1)
- earthquake source observations (1)
- eclogite (UHP) (1)
- eco-hydrological modelling (1)
- ecohydrology (1)
- ecological genetics (1)
- economic impacts (1)
- effective porosity (1)
- effektive Porosität (1)
- elastic properties (1)
- elastic rock properties (1)
- electric and magnetic fields (1)
- electrons (1)
- elektrische und magnetische Felder (1)
- elevated CO2 concentration (1)
- emergency response (1)
- energy demand (1)
- energy efficiency (1)
- enhanced geothermal system (1)
- enhanced geothermal systems (EGS) (1)
- environmental monitoring (1)
- environmental reconstruction (1)
- environmental seismology (1)
- eocene thermal maximum (1)
- epithermale Zinn-Silber-lagerstätte (1)
- equatorial electrojet (1)
- equatorial plasma depletions (1)
- ererbte Strukturen (1)
- erosion rates (1)
- estuary (1)
- evaporite minerals (1)
- evaporites (1)
- evapotranspiration (1)
- evolution (1)
- exhumation processes (1)
- exhumation rates (1)
- exposure (1)
- exposure age dating (1)
- extinction event (1)
- extracellular DNA (1)
- extreme Ereignisse (1)
- extreme Klimaereignisse (1)
- extreme hydro-meteorologische Ereignisse (1)
- extreme hydrometeorological events (1)
- extreme precipitation (1)
- failed rift (1)
- fallamiento activo (1)
- faltendes neuronales Netzwerk (1)
- fan (1)
- fatigue (1)
- fault (1)
- fault bend fold (1)
- fault healing (1)
- fault plane structure (1)
- fault reactivation (1)
- fault zone architecture (1)
- feldspar (1)
- ferropericlase (1)
- fieldwork (1)
- finite Differenzen (1)
- finite Elemente (1)
- finite difference simulation (1)
- finite differences (1)
- finite elements (1)
- fire emissions (1)
- fire history (1)
- fission track (1)
- fissure eruption (1)
- flash flood (1)
- flash floods (1)
- flat-slab subduction (1)
- flood (1)
- flood adaptation (1)
- flood events (1)
- flood mitigation (1)
- flood reconstruction (1)
- flood risk analysis (1)
- flood types (1)
- flood volcanism (1)
- flooding (1)
- floodplain (1)
- floodplain inundation (1)
- floodplains (1)
- fluctuations (1)
- fluid (1)
- fluid inclusions (1)
- fluid rock interaction (1)
- fluid-melt interaction (1)
- fluid-rock interactions (1)
- fluorescence imaging (1)
- fluvial fill terraces (1)
- fluvial incision (1)
- fluviale Einschneidung (1)
- flux tracking (1)
- fluxo de fluidos (1)
- focal mechanisms (1)
- folds (1)
- food web (1)
- foraminifera (1)
- fore-arc (1)
- forecast (1)
- foreland deformation (1)
- forest (1)
- forest conversion (1)
- forest management (1)
- forest structure (1)
- forestry (1)
- formation damage (1)
- foundation (1)
- fracture growth (1)
- fracture mechanics (1)
- fracture toughness (1)
- fracture transmissivity (1)
- fracture-controlled (1)
- frequency analysis (1)
- frictional properties (1)
- fundamental frequency (1)
- gabbros (1)
- gas geochemistry (1)
- gas hydrates (1)
- gas production (1)
- geführte Wellen (1)
- gegen den Uhrzeigersinn gerichtete Rotation von Krustenblöcken zwischen zwei überlappenden Riftsegmenten (1)
- gekoppelter Fluid-und Wärmetransport (1)
- gelatin (1)
- gemeinsame Inversion (1)
- geo-bio interaction (1)
- geodesy (1)
- geodynamic modeling (1)
- geodynamic models (1)
- geodynamische Modelle (1)
- geodynamische Modellierung (1)
- geohazards (1)
- geologic fault (1)
- geological hyperspectral image classification (1)
- geologische Störungen (1)
- geologische Verwerfung (1)
- geologische hyperspektrale Bildklassifikation (1)
- geomagnetic excursions (1)
- geomagnetic observatory data (1)
- geomagnetic storm drivers (1)
- geomagnetische Exkursionen (1)
- geomechanical modelling (1)
- geomechanics (1)
- geomechanische Modellierung (1)
- geophyics (1)
- geophysical methods (1)
- geophysikalische Methoden (1)
- geoquímica da alteração hidrotermal (1)
- geothermal (1)
- geothermal exploration (1)
- geothermal monitoring (1)
- geothermics (1)
- geothermische Exploration (1)
- geothermische Überwachung (1)
- geothermischer Reservoire (1)
- geschlossene Haubenmessmethode (1)
- gestreute Phasen (1)
- glacial hazards (1)
- glacial incision (1)
- glacial isostatic adjustment (1)
- glacial lake outburst floods (1)
- glacier (1)
- glacier forefield (1)
- glaciers (1)
- glass (1)
- glass structure (1)
- glasses (1)
- glaziale Einschneidung (1)
- global (1)
- global change (1)
- global flood model (1)
- global inversion (1)
- global monsoon (1)
- global navigation satellite systems (1)
- global vegetation model (1)
- globale Inversion (1)
- globale und lokale Muster des Klimas (1)
- globales Navigationssatellitensystem (1)
- globales Positionsbestimmungssystem (1)
- globales Überschwemmungsmodell (1)
- grain-size distribution (1)
- grandes movimientos en masa (1)
- granulite (1)
- graphite (1)
- gravimetry (1)
- grazing (1)
- green-green dilemma (1)
- greenhouse gases (1)
- gross primary production (1)
- ground motion modeling (1)
- ground motion variability (1)
- ground motions (1)
- ground penetrating radar (1)
- ground-motion modelling (1)
- ground-motion models (1)
- ground-penetrating radar (1)
- ground-penetration radar (1)
- groundwater evolution (1)
- groundwater level (1)
- groundwater recharge (1)
- groundwater surface water interaction (1)
- groundwater vulnerability (1)
- growing season (1)
- growth response (1)
- große Massenbewegungen (1)
- guided waves (1)
- gulf coastal plain (1)
- half-life (1)
- halophiles (1)
- hanging wall (1)
- hazard (1)
- hazard assessments (1)
- hazards (1)
- heat (1)
- heat-stress (1)
- helium (1)
- herzynische Orogenese (1)
- heterogeneity (1)
- heterozoan carbonates (1)
- heterozoisch (1)
- heuristic analysis (1)
- high latitudes (1)
- high pressure (1)
- high pressure relicts (1)
- high temperature rock deformation (1)
- high-P metamorphism (1)
- high-intensity industrialized agricultural production systems (1)
- high-pressure (1)
- high-pressure incubation system (1)
- high-pressure metasediments (1)
- high-resolution record (1)
- hillslope diffusion (1)
- hillslope hydrology (1)
- historical earthquakes (1)
- historical geomagnetic storms (1)
- historische Erdbeben (1)
- hochdruckmetamorphe Sedimente (1)
- hollow cylinder experiments (1)
- holocene (1)
- horizontal-vertikales Spektralverhältnis (1)
- horizontaler Fluss (1)
- host rock scale (1)
- huddle test (1)
- human impact (1)
- hybrid modelling (1)
- hydrate (1)
- hydrate formation (1)
- hydrate habitus (1)
- hydraulic simulation (1)
- hydraulische Risserzeugung (1)
- hydraulisches Aufbrechen (1)
- hydro-meteorological risk (1)
- hydro-meteorologische Risiken (1)
- hydro-meterological hazards (1)
- hydroclimatology (1)
- hydrogel (1)
- hydrogenase (1)
- hydrogeology (1)
- hydrogravimetry (1)
- hydrological flow paths (1)
- hydrological modeling (1)
- hydrological monitoring and modelling (1)
- hydrologische Fließpfade (1)
- hydrologische Vorbedingungen (1)
- hydropower (1)
- hydrothermal (1)
- hydrothermal systems (1)
- hydrothermale Alteration (1)
- hydrothermale Systeme (1)
- hyperspectral remote sensing (1)
- hyperspektral (1)
- hyperspektral Fernerkundung (1)
- ice (1)
- ice dam (1)
- ice dynamics (1)
- ice sheet (1)
- identifying influential nodes (1)
- image processing (1)
- impact (1)
- impact assessment (1)
- in-situ analysis (1)
- in-situ remediation (1)
- in-stream processes (1)
- incipient continent-continent collision (1)
- indischer Monsun (1)
- induced chlorophyll Fluorescence (1)
- induzierte Seismizität (1)
- induzierten Seismizität (1)
- inherited structures (1)
- injection (1)
- injection scheme (1)
- innovation (1)
- insights (1)
- instrumental seismology (1)
- instrumentelle Seismologie (1)
- insurance (1)
- inter- and intra-station variability (1)
- interferometric SAR (InSAR) (1)
- interferometry (1)
- intermontane Becken (1)
- intermontane Talverfüllungen (1)
- intermontane basin (1)
- intermontane valley fill (1)
- internal structure (1)
- introgression (1)
- inundation (1)
- inverse Modellierung (1)
- inverse Modellirung (1)
- inverse modeling (1)
- ionic conductivity (1)
- ionosphere (1)
- ionospheric scale lengths (1)
- iron reduction (1)
- iron-rich sediment (1)
- isostatic uplift (1)
- isostatische Hebung (1)
- isotopic composition (1)
- isotopic fractionation (1)
- isturbance tracking (1)
- joint inversion (1)
- kerogen kinetics (1)
- kimmerische Orogenese (1)
- kombinatorische inverse Modellierung (1)
- komplexe Systeme (1)
- kontinuierlicher Simulationsansatz (1)
- kosmische Neutronenstrahlung (1)
- kosmische Strahlung (1)
- kosmogen (1)
- kosmogene Radionuklid-basierte Datierung (1)
- kritische Zone (1)
- krustale Spannungen (1)
- künstliche neurale Netzwerke (1)
- lacustrine record (1)
- lacustrine sediment (1)
- lake Donggi Cona (1)
- lake Meerfelder Maar (1)
- lake basins (1)
- lake catchments (1)
- lake drainage (1)
- lake mixing (1)
- lake sediment (1)
- lake system responses (1)
- lakes water balance (1)
- lakustrine Abfolge (1)
- lamprophyre (1)
- land cover change (1)
- land use (1)
- land-use change (1)
- landforms (1)
- landscape preferences (1)
- landscape effects (1)
- landscape hydrology (1)
- landscape transience (1)
- larch species (1)
- large mass movements (1)
- laser heating (1)
- laser-geheizte Diamantstempelzelle (1)
- laser-heated Diamond Anvil Cell (1)
- last glacial period (1)
- late cenozoic stress field (1)
- late holocene (1)
- latitude ionosphere (1)
- lava fountains (1)
- lead (1)
- leaf wax (1)
- length measurements (1)
- lichenometry (1)
- lidar (1)
- lineare spektrale Entmischung (1)
- lipid biomarkers (1)
- lithium (1)
- lithosphere net rotation (1)
- lithosphere stress field (1)
- lithosphärisches Spannungsfeld (1)
- local Seismicity (1)
- localized deformation (1)
- localized flooding (1)
- logistic regression (1)
- lokale Seismitität (1)
- low flow (1)
- low molecular weight organic acids (1)
- low-intensity eco-agricultural production systems (1)
- lower crustal bodies (1)
- lower mantle (1)
- lower thermosphere (1)
- lunar tides (1)
- lunare Gezeiten (1)
- lysimeter (1)
- ländliche Entwicklung (1)
- macrophytes (1)
- magma assisted continental rifting (1)
- magma degassing (1)
- magma-poor (1)
- magmagestütztes kontinentales Rifting (1)
- magmatic (1)
- magmatic arc (1)
- magmatic-hydrothermal systems (1)
- magmatisch (1)
- magmatisch-hydrothermale Systeme (1)
- magmatism (1)
- magnesite (1)
- magnetic field (1)
- magnetic polarisation direction (1)
- magnetische Polarisationsrichtung (1)
- magnetosphere (1)
- magnetostratigraphy (1)
- magnetotelluric (1)
- manaderos de petróleo (1)
- mantle (1)
- margins (1)
- marine sediments (1)
- marine terrace (1)
- marine terraces (1)
- mass (1)
- mass extinction (1)
- mass wasting (1)
- matríz mineral (1)
- maturity-related biomarkers (1)
- mecanismos de disparo (1)
- mehrfache Stressfaktoren (1)
- melilitite (1)
- melt inclusions (1)
- melt structure (1)
- menschliche Einflüsse (1)
- metagenomic analysis (1)
- metal recycling plants (1)
- metaophiolite (1)
- metasomatism (1)
- meteoric 10Be (1)
- methane (1)
- microbial methane oxidation (1)
- microplate (1)
- microseismicity (1)
- microsructure (1)
- microstructural deformation mechanisms (1)
- microstructures (1)
- microtopography (1)
- microzonation (1)
- mid-latitude Westerlies (1)
- middle Miocene (1)
- middle atmosphere (1)
- migration (1)
- mikrobielle Gemeinschaften (1)
- mikrobielle aerobe Methanoxidation (1)
- mine face mapping (1)
- mineral composition (1)
- mineral mapping (1)
- mineral matrix (1)
- mineral reaction (1)
- mineral weathering reactions (1)
- mineralische Matrix (1)
- mitochondrial haplotypes (1)
- mittleres Miozän (1)
- mixture models (1)
- modelling error sources (1)
- modifizierte räumliche Autkorrelationsmethode (1)
- molecular biomarkers (1)
- molekulare Biomarker (1)
- molybdenum (1)
- moment tensors (1)
- monazite (1)
- mountain geomorphology (1)
- mountain hydrology (1)
- mountain rivers (1)
- mountainous rivers (1)
- multi-equilibrium thermobarometry (1)
- multi-hazard (1)
- multi-proxy approach (1)
- multi-slab (1)
- multi-stage exhumation (1)
- multiple stress factors (1)
- multiscale network (1)
- multispectral (1)
- multitemporal (1)
- multivariate Statistik (1)
- multivariate statistics (1)
- muscovite (1)
- music information retrieval (1)
- musical scales (1)
- musikalische Tonleitern (1)
- n-alkane (1)
- n-alkanes (1)
- nZVI (1)
- nachaltige Städteentwicklung (1)
- nachhaltige Entwicklung (1)
- nano zero-valent iron (1)
- nanoscale zero-valent iron (nZVI) (1)
- natural dams (1)
- natural hazard management (1)
- natural risks (1)
- natürlichen Ölaustritten (1)
- near-surface geophysics (1)
- near-vertical seismic reflection (1)
- nearshore zone (1)
- neodymium (1)
- neogene (1)
- neon (1)
- net ecosystem exchange (1)
- network (1)
- neutron field (1)
- neutrons (1)
- next generation sequencing (1)
- nicht-monetäre Bewertung (1)
- nichtisothermer Mehrphasenfluss (1)
- nightlights (1)
- nitrogen (1)
- noble gas (1)
- noble gas isotopes (1)
- noise cross (1)
- noise reduction (1)
- non-destructive testing (1)
- non-isothermal multiphase flow (1)
- non-monetary valuation (1)
- nonstationarity (1)
- normal faulting (1)
- north-atlantic (1)
- northern Andes (1)
- northern seward peninsula (1)
- nuclear waste disposal (1)
- nuclides (1)
- numerical (1)
- numerical models (1)
- numerisch (1)
- numerische Modelle (1)
- numerische Strömungsmechanik (1)
- nutrient emissions (1)
- nutrient retention (1)
- nutrients (1)
- nördliche Anden (1)
- nördliche hohe Breitengrade (1)
- oberflächennahe Geophysik (1)
- oberflächennahe Geophysík (1)
- object based image analysis (1)
- object-based damage modeling (1)
- object-based image analysis (1)
- objektbasierte Bildanalyse (1)
- observational seismology (1)
- occurrence rate (1)
- ocean acidification (1)
- oceanic crust (1)
- offene Daten (1)
- offener Tagebau (1)
- oil seeps (1)
- oligocene climate (1)
- onset times (1)
- open (1)
- open data (1)
- open pit mining (1)
- operational service (1)
- ophiolite (1)
- opinion (1)
- optical data (1)
- optical properties (1)
- optimal array configuration (1)
- optimale Array-Konfiguration (1)
- optische Eigenschaften (1)
- ore (1)
- ore deposit (1)
- organic carbon (1)
- organic matter (1)
- organischer Kohlenstoff (1)
- organisches Material (1)
- organofacies (1)
- origination (1)
- orogenic evolution (1)
- orogenic peridotite (1)
- orogeny (1)
- ortsverteile faseroptische Dehnungsmessung (1)
- ostafrikanisches Riftsystem (1)
- outburst floods (1)
- oxygen and carbon stable isotopes (1)
- oxygen isotope (1)
- oxygen isotopes (1)
- ozeanische Kruste (1)
- pH (1)
- palaeoclimatology (1)
- palaeoecology (1)
- palaeointensity (1)
- palaeolimnology (1)
- palaeomagnetism (1)
- paleo-lake Mweru (1)
- paleo-sediment (1)
- paleo-strain calculation (1)
- paleo-topography (1)
- paleoaltimetry (1)
- paleofloods (1)
- paleogeography (1)
- paleohydrology (1)
- paleolimnology (1)
- paleosecular variations (1)
- paleosol sequence (1)
- panafrican orogeny (1)
- panafrikanische Orogenese (1)
- parallel seismic (1)
- part 1 (1)
- participatory mapping (1)
- particle swarm optimisation (1)
- passive Seismik (1)
- passive microwave (1)
- passive seismic (1)
- pattern recognition (1)
- patterns (1)
- percolation (1)
- periglacial landscape evolution (1)
- periglacial landscapes (1)
- periglaziale Landschaften (1)
- periglaziale Landschaftsentwicklung (1)
- permafrost degradation (1)
- permafrost disturbances (1)
- permafrost ecosystems (1)
- permafrost landscapes (1)
- permafrost regions (1)
- permafrost sediments (1)
- permafrost thaw (1)
- permafrost thaw disturbances (1)
- permanent deformation (1)
- permanente Verformung (1)
- permeability (1)
- permeability evolution (1)
- permeability test (1)
- petrology (1)
- petrothermal systems (1)
- petrothermale Systeme (1)
- petrothermales System (EGS) (1)
- phasepicker (1)
- phytoplankton distribution (1)
- picker (1)
- pile (1)
- plant ecology (1)
- plant waxes (1)
- plant-habitat interactions (1)
- plate boundary friction (1)
- plate motions (1)
- plate tectonics (1)
- plateau uplift (1)
- plum (1)
- plume (1)
- plume-ridge interaction (1)
- pluvial flooding (1)
- pluvial floods (1)
- plötzliche stratosphärische Erwärmungsereignisse (1)
- point cloud (1)
- polar ice (1)
- polares Eis (1)
- polarimetric decompositions (1)
- polarimetrische Dekompositionen (1)
- pollen (1)
- pollution (1)
- pollution indices (1)
- poly(lactic acid) (1)
- polymictic lakes (1)
- polymiktische Seen (1)
- polynya (1)
- porphyry copper deposit (1)
- potentially affected areas (PAA) (1)
- potentially toxic elements (1)
- precision horticulture (1)
- pressure solution (1)
- pressures (1)
- principal components (1)
- prior derivation (1)
- probabilistic approach (1)
- probabilistic approaches (1)
- probabilistischer Ansatz (1)
- process identification (1)
- production rates (1)
- productivity (1)
- propagation (1)
- psychology (1)
- quantitative data (1)
- quartäre Geochronologie (1)
- quaternary (1)
- radar satellite interferometry (1)
- radiación y propiedades químicas (1)
- radial flow (1)
- radiale Strömung (1)
- radiation and chemical properties (1)
- radiation-damage (1)
- radiocarbon age dating (1)
- radiogene Wärmeproduktion (1)
- radiogenic heat production (1)
- radiogenic heat-production (1)
- radiogenic isotopes (1)
- radiolyse (1)
- radiolysis (1)
- radiólisis (1)
- railway infrastructure (1)
- railway transportation (1)
- rainfall (1)
- rainstorm (1)
- ramp (1)
- random vibration (1)
- range shifts (1)
- rapid damage mapping (1)
- rapid earthquake impact assessment (1)
- rate-state friction (1)
- reaction path modelling (1)
- reactivation (1)
- reactive transport groundwater model (1)
- reactive transport simulation (1)
- reaktive Transportsimulation (1)
- reaktives Grundwassermodell (1)
- real-time application (1)
- recovery (1)
- recurrence (1)
- recurrence network (1)
- recurrence plot (1)
- recycling (1)
- reduction (1)
- reef (1)
- reflection (1)
- reflection seismics (1)
- reflection seismology (1)
- regimes (1)
- regionale Hydrologie (1)
- regionales Klimamodell (1)
- regression analysis (1)
- regularization (1)
- release (1)
- remediation (1)
- remote sensing data (1)
- renewable energy (1)
- required minimum runoff (1)
- reservoir (1)
- residential buildings (1)
- residuals (1)
- resources (1)
- response spectra (1)
- response time (1)
- retrogressive thaw slump (1)
- retrogressiven Auftaurutschungen (1)
- rheology (1)
- rhizosphere (1)
- ridge subduction (1)
- ridge-collision (1)
- rift (1)
- rift segments interaction (1)
- ring-fault (1)
- riparian zone (1)
- risk analysis (1)
- risk assessment (1)
- risk management cycle (1)
- risk model chain (1)
- river discharge (1)
- river sediment (1)
- rivers (1)
- rock fracture (1)
- rock glaciers (1)
- rock mass (1)
- rock mechanics (1)
- rock-water interaction (1)
- rockmagnetism (1)
- rockslide (1)
- rotation (1)
- rotational seismology (1)
- roughness (1)
- rupture (1)
- rural development (1)
- russische Arktis (1)
- rutile-type (1)
- räumlich explizit (1)
- räumliche Aggregation (1)
- räumliche Analyse (1)
- räumliche Autkorrelationsmethode (1)
- räumliche Autokorrelation (1)
- räumliche Kalibrierung (1)
- räumliche Variabilität (1)
- räumliche Wiederkehr (1)
- saisonale Arbeitsmigration (1)
- saline Seen (1)
- saline lakes (1)
- saline pan (1)
- saline pan cycle (1)
- salt dissolution (1)
- salt rock (1)
- san andreas fault (1)
- sandstones (1)
- saprolite (1)
- satellite images (1)
- savanna (1)
- savanna ecology (1)
- scattered phases (1)
- scatterer location (1)
- scenario (1)
- schnelle Einschätzung von Erdbebenauswirkungen (1)
- sea (1)
- sea-level projections (1)
- seasonal labor migration (1)
- seasonality (1)
- sedaDNA (1)
- sediment (1)
- sediment fingerprinting (1)
- sediment routing (1)
- sediment source fingerprinting (1)
- sediment thickness (1)
- sediment transit time (1)
- sediment transport (1)
- sediment transport modelling (1)
- sediment trap (1)
- sediment volume (1)
- sediment-routing system (1)
- sedimentary ancient DNA (1)
- sedimentary basin (1)
- sedimentary basins (1)
- sedimentary dynamics (1)
- sedimentary environments (1)
- sedimentary facies (1)
- sedimentary microbes (1)
- sedimentary organic matter (1)
- sedimentary record (1)
- sedimentation pattern (1)
- sedimentology (1)
- sediments (1)
- sedimentäre Systeme (1)
- sedimentäre alte DNA (1)
- seismic (1)
- seismic array (1)
- seismic attenuation (1)
- seismic attributes (1)
- seismic cycle modeling (1)
- seismic event localization (1)
- seismic imaging (1)
- seismic interferometry (1)
- seismic interpretation (1)
- seismic measurements (1)
- seismic monitoring (1)
- seismic sequence stratigraphy (1)
- seismic signal processing (1)
- seismic source inversion (1)
- seismic source-time function estimation (1)
- seismic velocities (1)
- seismic velocity (1)
- seismicity and tectonics (1)
- seismicity modelling (1)
- seismics (1)
- seismische Attribute (1)
- seismische Dämpfung (1)
- seismische Ereignislokalisierung (1)
- seismische Geschwindigkeit (1)
- seismische Geschwindigkeiten (1)
- seismische Interpretation (1)
- seismische Messungen (1)
- seismische Rauschen (1)
- seismische Sequenzstratigraphie (1)
- seismische Stapelungs-Methode (1)
- seismische Tomographie (1)
- seismisches Array (1)
- seismogene Kopplungszone (1)
- seismogenic coupling zone (1)
- seismology ; PKP caustic point B ; diffraction of PKP core phases ; decay spectra of waveform data ; transition zone to the earth's inner core ; Germa (1)
- seismotectonic (1)
- seltene Erden (1)
- sensors (1)
- shadow detection (1)
- shale strength (1)
- shallow geophysics (1)
- shallow-water carbonates (1)
- shear zones (1)
- shoreline (1)
- shorelines (1)
- shotgun sequencing (1)
- signal formation (1)
- silicate melt (1)
- silicate melts (1)
- silicate weathering (1)
- silicon (1)
- silikatische Schmelzen (1)
- simulation on a day-to-day-basis (1)
- simulation-based attribution (1)
- simulações numéricas (1)
- singleslab (1)
- sistemas magmático-hidrotermais (1)
- site characterization (1)
- skarn (1)
- skill (1)
- slags (1)
- slope failure (1)
- small baseline subset (SBAS) (1)
- snow avalanches (1)
- snow detection (1)
- social (1)
- soil constituents mapping (1)
- soil heterogeneity (1)
- soil hydrology (1)
- soil landscape (1)
- soil moisture patterns (1)
- soil water content (1)
- soils (1)
- sorption (1)
- source array (1)
- source array optimal design (1)
- source direction (1)
- source duration (1)
- source model (1)
- source parameters (1)
- source-to-sink (1)
- southern Turkey (1)
- spatial aggregation (1)
- spatial analyses (1)
- spatial autocorrelation (1)
- spatial calibration (1)
- spatial correlation (1)
- spatial recurrence (1)
- spatial scales (1)
- spatial variability (1)
- spatial-distribution (1)
- spatially explicit (1)
- special sensor microwave imager (1)
- special sensor microwave imager/sounder (1)
- spectral adjustment (1)
- spectral unmixing (1)
- spectro-directional (1)
- spektro-direktional (1)
- spherical harmonics (1)
- spread F (1)
- spröde Deformation (1)
- spätes Holozän (1)
- stabilen Isotopen (1)
- stable isotope (1)
- stalagmites (1)
- starker Konvektion (1)
- state-transition models (1)
- statistical seismology (1)
- statistische Seismologie (1)
- steep-angle analysis of PcP (1)
- stochastic algorithms (1)
- stratigraphic forward modelling (1)
- stratigraphische Vorwärtsmodellierung (1)
- stratigraphy (1)
- streambed morphology (1)
- streamflow variability (1)
- strength (1)
- stress (1)
- stress changes (1)
- stress measurement (1)
- stress modeling (1)
- stress partitioning (1)
- stress pattern (1)
- strike-slip (1)
- strike-slip faults (1)
- structural inheritance (1)
- structural modelling (1)
- structure from motion (1)
- strukturelle Kontrolle (1)
- subduction earthquake (1)
- subduction-accretionary complexes (1)
- subduktions-akkretions Komplexe (1)
- subrosion (1)
- subsidence analysis (1)
- subsidence history (1)
- subsurface (1)
- subsurface biosphere (1)
- sudden stratospheric warming (1)
- sulfate reduction (1)
- sulphate reduction (1)
- summer monsoon (1)
- superconducting gravimeter (SG) (1)
- supervised machine learning (1)
- surface (1)
- surface evolution (1)
- surface exposure dating (1)
- surface reflectance (1)
- surface urban heat island effect (1)
- surface water flooding (1)
- susceptibility of the European electricity sector (1)
- suspended sediments (1)
- sustainable development (1)
- sustainable urban development (1)
- sustained casing pressure (1)
- suture zones (1)
- swarm mission (1)
- switzerland (1)
- synchronization (1)
- syntaxis (1)
- synthetic array beam power (1)
- synthetic hydrate samples (1)
- synthetic sandstone (1)
- synthetic seismograms (1)
- synthetische Array-Strahlleistung (1)
- synthetische Hydratproben (1)
- synthetische Seismogramme (1)
- systems (1)
- tagesaktuelle Simulation (1)
- tectonic evolution (1)
- tectonic inversion (1)
- tectonic stress (1)
- tectonic uplift (1)
- tektonische Hebung (1)
- tektonische Spannungen (1)
- teleseismic rupture tracking (1)
- teleseismische Bruchverfolgung (1)
- temperature changes (1)
- temperature field analysis (1)
- temporal gravity variations (1)
- tensile Anteile (1)
- tensile earthquake (1)
- tensile earthquakes (1)
- terrigenous input (1)
- theory (1)
- thermal conductivity (1)
- thermal model (1)
- thermal modelling (1)
- thermal properties (1)
- thermisches Feld (1)
- thermisches Modell (1)
- thermo-mechanical modeling (1)
- thermo-mechanics (1)
- thermo-mechanische Modellierung (1)
- thermobarometry (1)
- thermochemical mantle convection (1)
- thermochemischer Mantelkonvektion (1)
- thermodynamic and kinetic properties (1)
- thermodynamic modelling (1)
- thermodynamische Modellierungen (1)
- thermodynamische und kinetische Eigenschaften (1)
- thermoerosion (1)
- thermokarst lakes (1)
- thermokarst processes (1)
- thickness-displacement relationships (1)
- thrust belts (1)
- tibetan plateau (1)
- tide gauge observations (1)
- tiefer Kohlenstoff (1)
- tiefes Lernen (1)
- time dependent (1)
- time scale (1)
- time-scale (1)
- time-series analysis (1)
- time-series mapping (1)
- tin (1)
- tomography (1)
- topography (1)
- tourmaline (1)
- trace element partitioning (1)
- traditional Georgian music (1)
- traditionelle Georgische Musik (1)
- transferability (1)
- transform fault (1)
- transformation of hydrological signals (1)
- transient earthquake patterns (1)
- transiente Erdbebenmuster (1)
- transit-time (1)
- transnational migration (1)
- transnationale Migration (1)
- transnationalism (1)
- transport processes (1)
- travel time distributions (1)
- traveltime (1)
- tree water status (1)
- treeline (1)
- trend analyses (1)
- trend attribution (1)
- trend detection (1)
- trend drivers (1)
- triaxial deformation experiments (1)
- triaxiale Deformationsexperimente (1)
- trigger mechanism (1)
- tritium assay (1)
- tropical biodiversity (1)
- tropical swamp (1)
- tsunami early warning (1)
- tsunami risk (1)
- tundra (1)
- tundra–taiga ecotone (1)
- tungsten-tin deposits (1)
- turbidity modelling (1)
- turmalina (1)
- typhoons (1)
- ultra-low velocity zones (1)
- ultrasound (1)
- uncertainties (1)
- uncertainty estimation (1)
- unconventional shale (1)
- underground coal gasification (1)
- united states (1)
- unkonventionelle Schiefer (1)
- unterer Mantel (1)
- upper mantle density heterogeneities (1)
- upper mantle viscosity structure (1)
- uranium (1)
- uranium-lead-dating (1)
- urban development (1)
- urban efficiency (1)
- urban form (1)
- urban heat island effect (1)
- urban infill development (1)
- varve (1)
- varved sediments (1)
- vegetation cover (1)
- vegetation history (1)
- vegetation states (1)
- vegetation trajectories (1)
- vegetation-climate feedbacks (1)
- vegetation‐climate‐fire‐soil feedbacks (1)
- velocity model (1)
- velocity structure (1)
- verbesserte geothermische Systeme (1)
- verstärkende Seen (1)
- vertical coupling (1)
- vertikale Kuppelung (1)
- vertikaler Fluss (1)
- very slow moving landslide (1)
- video analysis (1)
- virtual active seismic (1)
- virtuelle aktive Seismik (1)
- volcanic glass (1)
- volcanic hazard assessment (1)
- volcanic hydrothermal systems (1)
- volcanic seismology (1)
- volcanic tremor (1)
- volcaniclastics (1)
- volcanism (1)
- volcano deformation (1)
- volcano remote sensing (1)
- volcano seismology (1)
- volcanology (1)
- voring basin (1)
- vulkanische Entgasungs-und Hydrothermalsysteme (1)
- vulkanische Entgasungssysteme (1)
- vulkanischer Gläser (1)
- vulkanischer Tremor (1)
- wasting (1)
- water age (1)
- water balance model (1)
- water budget (1)
- water fluxes (1)
- water monitoring (1)
- water quality (1)
- water quality modelling (1)
- water resources (1)
- water rock interactions (1)
- water storage changes (1)
- water vapour (1)
- wave scattering and diffraction (1)
- wave velocities (1)
- weakening mechanisms (1)
- weather (1)
- weather pattern (1)
- weather patterns (1)
- weathering feedback (1)
- wetland (1)
- wetlands (1)
- wind energy production (1)
- wind energy-biodiversity (1)
- wind gusts (1)
- winderosion (1)
- winds (1)
- winter (1)
- wood compost (1)
- x-ray absorption spectroscopy (1)
- zeitabhängige Gravitationsvariation (1)
- zentral-östliches Beringia (1)
- zentrale Anden (1)
- zentralen Anden (1)
- zinc (1)
- zirkulare Statistik (1)
- Ästuar (1)
- Ätna (1)
- Ökohydrologie (1)
- Östliches Karoo-Becken (1)
- Überschwemmungen (1)
- Überschwemmungsflächen (1)
- Überwachung (1)
- Þeistareykir Iceland (1)
- Þeistareykir Island (1)
- äquatorialen Plasma-Verarmungen (1)
- äquatorialer Elektrojet (1)
- ökohydrologische Modellierung (1)
- ökologische Modellierung (1)
- ökonomische Auswirkungen (1)
- östlich-südzentrale Anden (1)
- östliche Kordillere (1)
- δ18O and δ13C stabile Isotope (1)
- δ18O and δ13C stable isotopes (1)
Institute
- Institut für Geowissenschaften (508) (remove)
Strong hydroclimatic controls on vulnerability to subsurface nitrate contamination across Europe
(2020)
Subsurface contamination due to excessive nutrient surpluses is a persistent and widespread problem in agricultural areas across Europe. The vulnerability of a particular location to pollution from reactive solutes, such as nitrate, is determined by the interplay between hydrologic transport and biogeochemical transformations. Current studies on the controls of subsurface vulnerability do not consider the transient behaviour of transport dynamics in the root zone. Here, using state-of-the-art hydrologic simulations driven by observed hydroclimatic forcing, we demonstrate the strong spatiotemporal heterogeneity of hydrologic transport dynamics and reveal that these dynamics are primarily controlled by the hydroclimatic gradient of the aridity index across Europe. Contrasting the space-time dynamics of transport times with reactive timescales of denitrification in soil indicate that similar to 75% of the cultivated areas across Europe are potentially vulnerable to nitrate leaching for at least onethird of the year. We find that neglecting the transient nature of transport and reaction timescale results in a great underestimation of the extent of vulnerable regions by almost 50%. Therefore, future vulnerability and risk assessment studies must account for the transient behaviour of transport and biogeochemical transformation processes.
Rapidly growing seismic and macroseismic databases and simplified access to advanced machine learning methods have in recent years opened up vast opportunities to address challenges in engineering and strong motion seismology from novel, datacentric perspectives. In this thesis, I explore the opportunities of such perspectives for the tasks of ground motion modeling and rapid earthquake impact assessment, tasks with major implications for long-term earthquake disaster mitigation.
In my first study, I utilize the rich strong motion database from the Kanto basin, Japan, and apply the U-Net artificial neural network architecture to develop a deep learning based ground motion model. The operational prototype provides statistical estimates of expected ground shaking, given descriptions of a specific earthquake source, wave propagation paths, and geophysical site conditions. The U-Net interprets ground motion data in its spatial context, potentially taking into account, for example, the geological properties in the vicinity of observation sites. Predictions of ground motion intensity are thereby calibrated to individual observation sites and earthquake locations.
The second study addresses the explicit incorporation of rupture forward directivity into ground motion modeling. Incorporation of this phenomenon, causing strong, pulse like ground shaking in the vicinity of earthquake sources, is usually associated with an intolerable increase in computational demand during probabilistic seismic hazard analysis (PSHA) calculations. I suggest an approach in which I utilize an artificial neural network to efficiently approximate the average, directivity-related adjustment to ground motion predictions for earthquake ruptures from the 2022 New Zealand National Seismic Hazard Model. The practical implementation in an actual PSHA calculation demonstrates the efficiency and operational readiness of my model. In a follow-up study, I present a proof of concept for an alternative strategy in which I target the generalizing applicability to ruptures other than those from the New Zealand National Seismic Hazard Model.
In the third study, I address the usability of pseudo-intensity reports obtained from macroseismic observations by non-expert citizens for rapid impact assessment. I demonstrate that the statistical properties of pseudo-intensity collections describing the intensity of shaking are correlated with the societal impact of earthquakes. In a second step, I develop a probabilistic model that, within minutes of an event, quantifies the probability of an earthquake to cause considerable societal impact. Under certain conditions, such a quick and preliminary method might be useful to support decision makers in their efforts to organize auxiliary measures for earthquake disaster response while results from more elaborate impact assessment frameworks are not yet available.
The application of machine learning methods to datasets that only partially reveal characteristics of Big Data, qualify the majority of results obtained in this thesis as explorative insights rather than ready-to-use solutions to real world problems. The practical usefulness of this work will be better assessed in the future by applying the approaches developed to growing and increasingly complex data sets.
We present a new set of global and local sea‐level projections at example tide gauge locations under the RCP2.6, RCP4.5, and RCP8.5 emissions scenarios. Compared to the CMIP5‐based sea‐level projections presented in IPCC AR5, we introduce a number of methodological innovations, including (i) more comprehensive treatment of uncertainties, (ii) direct traceability between global and local projections, and (iii) exploratory extended projections to 2300 based on emulation of individual CMIP5 models. Combining the projections with observed tide gauge records, we explore the contribution to total variance that arises from sea‐level variability, different emissions scenarios, and model uncertainty. For the period out to 2300 we further breakdown the model uncertainty by sea‐level component and consider the dependence on geographic location, time horizon, and emissions scenario. Our analysis highlights the importance of local variability for sea‐level change in the coming decades and the potential value of annual‐to‐decadal predictions of local sea‐level change. Projections to 2300 show a substantial degree of committed sea‐level rise under all emissions scenarios considered and highlight the reduced future risk associated with RCP2.6 and RCP4.5 compared to RCP8.5. Tide gauge locations can show large ( > 50%) departures from the global average, in some cases even reversing the sign of the change. While uncertainty in projections of the future Antarctic ice dynamic response tends to dominate post‐2100, we see substantial differences in the breakdown of model variance as a function of location, time scale, and emissions scenario.
Lake sediments are increasingly explored as reliable paleoflood archives. In addition to established flood proxies including detrital layer thickness, chemical composition, and grain size, we explore stable oxygen and carbon isotope data as paleoflood proxies for lakes in catchments with carbonate bedrock geology. In a case study from Lake Mondsee (Austria), we integrate high-resolution sediment trapping at a proximal and a distal location and stable isotope analyses of varved lake sediments to investigate flood-triggered detrital sediment flux. First, we demonstrate a relation between runoff, detrital sediment flux, and isotope values in the sediment trap record covering the period 2011-2013 CE including 22 events with daily (hourly) peak runoff ranging from 10 (24) m(3) s(-1) to 79 (110) m(3) s(-1). The three- to ten-fold lower flood-triggered detrital sediment deposition in the distal trap is well reflected by attenuated peaks in the stable isotope values of trapped sediments. Next, we show that all nine flood-triggered detrital layers deposited in a sediment record from 1988 to 2013 have elevated isotope values compared with endogenic calcite. In addition, even two runoff events that did not cause the deposition of visible detrital layers are distinguished by higher isotope values. Empirical thresholds in the isotope data allow estimation of magnitudes of the majority of floods, although in some cases flood magnitudes are overestimated because local effects can result in too-high isotope values. Hence we present a proof of concept for stable isotopes as reliable tool for reconstructing flood frequency and, although with some limitations, even for flood magnitudes.
Diet analysis of bats killed at wind turbines suggests large-scale losses of trophic interactions
(2022)
Agricultural practice has led to landscape simplification and biodiversity decline, yet recently, energy-producing infrastructures, such as wind turbines, have been added to these simplified agroecosystems, turning them into multi-functional energy-agroecosystems. Here, we studied the trophic interactions of bats killed at wind turbines using a DNA metabarcoding approach to shed light on how turbine-related bat fatalities may possibly affect local habitats. Specifically, we identified insect DNA in the stomachs of common noctule bats (Nyctalus noctula) killed by wind turbines in Germany to infer in which habitats these bats hunted. Common noctule bats consumed a wide variety of insects from different habitats, ranging from aquatic to terrestrial ecosystems (e.g., wetlands, farmland, forests, and grasslands). Agricultural and silvicultural pest insects made up about 20% of insect species consumed by the studied bats. Our study suggests that the potential damage of wind energy production goes beyond the loss of bats and the decline of bat populations. Bat fatalities at wind turbines may lead to the loss of trophic interactions and ecosystem services provided by bats, which may add to the functional simplification and impaired crop production, respectively, in multi-functional ecosystems.
The sediment profile from Lake Goscia(z) over dot in central Poland comprises a continuous, seasonally resolved and exceptionally well-preserved archive of the Younger Dryas (YD) climate variation. This provides a unique opportunity for detailed investigation of lake system responses during periods of rapid climate cooling (YD onset) and warming (YD termination). The new varve record of Lake Goscia(z) over dot presented here spans 1662 years from the late Allerod (AL) to the early Preboreal (PB). Microscopic varve counting provides an independent chronology with a YD duration of 1149+14/-22 years, which confirms previous results of 1140 +/- 40 years. We link stable oxygen isotopes and chironomid-based air temperature reconstructions with the response of various geochemical and varve microfacies proxies especially focusing on the onset and termination of the YD. Cooling at the YD onset lasted similar to 180 years, which is about a century longer than the terminal warming that was completed in similar to 70 years. During the AL/YD transition, environmental proxy data lagged the onset of cooling by similar to 90 years and revealed an increase of lake productivity and internal lake re-suspension as well as slightly higher detrital sediment input. In contrast, rapid warming and environmental changes during the YD/PB transition occurred simultaneously. However, initial changes such as declining diatom deposition and detrital input occurred already a few centuries before the rapid warming at the YD/PB transition. These environmental changes likely reflect a gradual increase in summer air temperatures already during the YD. Our data indicate complex and differing environmental responses to the major climate changes related to the YD, which involve different proxy sensitivities and threshold processes.
Large rock slope failures play a pivotal role in long-term landscape evolution and are a major concern in land use planning and hazard aspects. While the failure phase and the time immediately prior to failure are increasingly well studied, the nature of the preparation phase remains enigmatic. This knowledge gap is due, to a large degree, to difficulties associated with instrumenting high mountain terrain and the local nature of classic monitoring methods, which does not allow integral observation of large rock volumes. Here, we analyse data from a small network of up to seven seismic sensors installed during July-October 2018 (with 43 days of data loss) at the summit of the Hochvogel, a 2592 m high Alpine peak. We develop proxy time series indicative of cyclic and progressive changes of the summit. Modal analysis, horizontal-to-vertical spectral ratio data and end-member modelling analysis reveal diurnal cycles of increasing and decreasing coupling stiffness of a 260,000 m(3) large, instable rock volume, due to thermal forcing. Relative seismic wave velocity changes also indicate diurnal accumulation and release of stress within the rock mass. At longer time scales, there is a systematic superimposed pattern of stress increased over multiple days and episodic stress release within a few days, expressed in an increased emission of short seismic pulses indicative of rock cracking. Our data provide essential first order information on the development of large-scale slope instabilities towards catastrophic failure. (c) 2020 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd
The Big Naryn Complex (BNC) in the East Djetim-Too Range of the Kyrgyz Middle Tianshan block is a tectonized, at least 2 km thick sequence of predominantly felsic to intermediate volcanic rocks intruded by porphyric rhyolite sills. It overlies a basement of metamorphic rocks and is overlain by late Neoproterozoic Djetim-Too Formation sediments; these also occur as tectonic intercalations in the BNC. The up to ca. 1100 m thick Lower Member is composed of predominantly rhyolites-to-dacites and minor basalts, while the at least 900 m thick pyroclastic Upper Member is dominated by rhyolitic-to-dacitic ignimbrites. Porphyric rhyolite sills are concentrated at the top of the Lower Member. A Lower Member rhyolite and a sill sample have LA-ICP-MS U-Pb zircon crystallization ages of 726.1 +/- 2.2 Ma and 720.3 +/- 6.5 Ma, respectively, showing that most of the magmatism occurred within a short time span in the late Tonian-early Cryogenian. Inherited zircons in the sill sample have Neoarchean (2.63, 2.64 Ga), Paleo- (2.33-1.81 Ga), Meso- (1.55 Ga), and Neoproterozoic (ca. 815 Ma) ages, and were derived from a heterogeneous Kuilyu Complex basement. A 1751 +/- 7 Ma Ar-40/Ar-39 age for amphibole from metagabbro is the age of cooling subsequent to Paleoproterozoic metamorphism of the Kuilyu Complex. The large amount of pyroclastic rocks, and their major and trace element compositions, the presence of Neoarchean to Neoproterozoic inherited zircons and a depositional basement of metamorphic rocks point to formation of the BNC in a continental magmatic arc setting.
The Salt Range in Pakistan exposes Precambrian to Pleistocene strata outcropping along the Salt Range Thrust (SRT). To better understand the in-situ Cambrian and Pliocene tectonic evolution of the Pakistan Subhimalaya, we have conducted low-temperature thermochronological analysis using apatite (U-Th-Sm)/He and fission track dating. We combine cooling ages from different samples located along the thrust front of the SRT into a thermal model that shows two major cooling events associated with rifting and regional erosion in the Late Palaeozoic and SRT activity since the Pliocene. Our results suggest that the SRT maintained a long-term average shortening rate of similar to 5-6 mm/yr and a high exhumation rate above the SRT ramp since similar to 4 Ma.
The simulation of broad-band (0.1 to 10 + Hz) ground-shaking over deep and spatially extended sedimentary basins at regional scales is challenging. We evaluate the ground-shaking of a potential M 6.5 earthquake in the southern Lower Rhine Embayment, one of the most important areas of earthquake recurrence north of the Alps, close to the city of Cologne in Germany. In a first step, information from geological investigations, seismic experiments and boreholes is combined for deriving a harmonized 3D velocity and attenuation model of the sedimentary layers. Three alternative approaches are then applied and compared to evaluate the impact of the sedimentary cover on ground-motion amplification. The first approach builds on existing response spectra ground-motion models whose amplification factors empirically take into account the influence of the sedimentary layers through a standard parameterization. In the second approach, site-specific 1D amplification functions are computed from the 3D basin model. Using a random vibration theory approach, we adjust the empirical response spectra predicted for soft rock conditions by local site amplification factors: amplifications and associated ground-motions are predicted both in the Fourier and in the response spectra domain. In the third approach, hybrid physics-based ground-motion simulations are used to predict time histories for soft rock conditions which are subsequently modified using the 1D site-specific amplification functions computed in method 2. For large distances and at short periods, the differences between the three approaches become less notable due to the significant attenuation of the sedimentary layers. At intermediate and long periods, generic empirical ground-motion models provide lower levels of amplification from sedimentary soils compared to methods taking into account site-specific 1D amplification functions. In the near-source region, hybrid physics-based ground-motions models illustrate the potentially large variability of ground-motion due to finite source effects.
Borehole leakage is a common and complex issue. Understanding the fluid flow characteristics of a cemented area inside a borehole is crucial to monitor and quantify the wellbore integrity as well as to find solutions to minimise existing leakages. In order to improve our understanding of the flow behaviour of cemented boreholes, we investigated experimental data of a large-scale borehole leakage tests by means of numerical modelling using three different conceptual models. The experiment was performed with an autoclave system consisting of two vessels bridged by a cement-filled casing. After a partial bleed-off at the well-head, a sustained casing pressure was observed due to fluid flow through the cementsteel composite. The aim of our simulations is to investigate and quantify the permeability of the cement-steel composite. From our model results, we conclude that the flow occurred along a preferential flow path at the cement-steel interface. Thus, the inner part of the cement core was impermeable during the duration of the experiment. The preferential flow path can be described as a highly permeable and highly porous area with an aperture of about 5 mu m and a permeability of 3 . 10(-12) m(2) (3 Darcy). It follows that the fluid flow characteristics of a cemented area inside a borehole cannot be described using one permeability value for the entire cement-steel composite. Furthermore, it can be concluded that the quality of the cement and the filling process regarding the cement-steel interface is crucial to minimize possible well leakages.
The southern Central Andes (SCA) (between 27 degrees S and 40 degrees S) is bordered to the west by the convergent margin between the continental South American Plate and the oceanic Nazca Plate. The subduction angle along this margin is variable, as is the deformation of the upper plate. Between 33 degrees S and 35 degrees S, the subduction angle of the Nazca plate increases from sub-horizontal (< 5 degrees) in the north to relatively steep (similar to 30 degrees) in the south. The SCA contain inherited lithological and structural heterogeneities within the crust that have been reactivated and overprinted since the onset of subduction and associated Cenozoic deformation within the Andean orogen. The distribution of the deformation within the SCA has often been attributed to the variations in the subduction angle and the reactivation of these inherited heterogeneities. However, the possible influence that the thickness and composition of the continental crust have had on both short-term and long-term deformation of the SCA is yet to be thoroughly investigated. For our investigations, we have derived density distributions and thicknesses for various layers that make up the lithosphere and evaluated their relationships with tectonic events that occurred over the history of the Andean orogeny and, in particular, investigated the short- and long-term nature of the present-day deformation processes. We established a 3D model of lithosphere beneath the orogen and its foreland (29 degrees S-39 degrees S) that is consistent with currently available geological and geophysical data, including the gravity data. The modelled crustal configuration and density distribution reveal spatial relationships with different tectonic domains: the crystalline crust in the orogen (the magmatic arc and the main orogenic wedge) is thicker (similar to 55 km) and less dense (similar to 2900 kg/m(3)) than in the forearc (similar to 35 km, similar to 2975 kg/m(3)) and foreland (similar to 30 km, similar to 3000 kg/m(3)). Crustal thickening in the orogen probably occurred as a result of stacking of low-density domains, while density and thickness variations beneath the forearc and foreland most likely reflect differences in the tectonic evolution of each area following crustal accretion. No clear spatial relationship exists between the density distribution within the lithosphere and previously proposed boundaries of crustal terranes accreted during the early Paleozoic. Areas with ongoing deformation show a spatial correlation with those areas that have the highest topographic gradients and where there are abrupt changes in the average crustal-density contrast. This suggests that the short-term deformation within the interior of the Andean orogen and its foreland is fundamentally influenced by the crustal composition and the relative thickness of different crustal layers. A thicker, denser, and potentially stronger lithosphere beneath the northern part of the SCA foreland is interpreted to have favoured a strong coupling between the Nazca and South American plates, facilitating the development of a sub-horizontal slab.
Dentro de la cuenca intermontana de Quito-Guay llabamba de Ecuador, se han identificado y analizado en este estudio, cinco depósitos coluviales inusualmente grandes de antiguos deslizamientos. El gran deslizamiento rotacional MM-5 Guayllabamba es el más extenso, con un volumen de 1183 millones de m3. Las mega avalanchas de escombros MM-1 Conocoto, MM-3 Oyacoto, y MM-4 San Francisco fueron desencadenadas originalmente por una ruptura inicial que estuvo asociada a un deslizamiento rotacional, los depósitos correspondientes tienen volúmenes entre 399 a 317 millones de m3. Finalmente, el depósito de menor volumen, el deslizamiento rotacional y caída de detritos MM-2 Batán, tiene un volumen de 8,7 millones de m3. En esta tesis, se realizó un estudio detallado de estos grandes movimientos en masa utilizando métodos neotectónicos y lito-tefrostratigráficos para comprender las condiciones geológicas y geomorfológicas de contorno que podrían ser relevantes para desencadenar estos movimientos en masa. La parte neotectónica del estudio se basó en el análisis geomorfológico cualitativo y cuantitativo de estos grandes depósitos de movimientos en masa, a través de la caracterización estructural de anticlinales ubicados al este de la subcuenca de Quito y sus flancos colapsados que constituyen las áreas de ruptura. Esta parte del análisis fue además apoyada por la aplicación de diferentes índices morfométricos para revelar procesos de evolución del paisaje forzados tectónicamente que pueden haber contribuido a la generación de movimientos en masa. La parte lito-tefrostratigráfica del estudio se basó en el análisis de las características petrográficas, geoquímicas y geocronológicas de los horizontes del suelo y de las cenizas volcánicas intercaladas, con el objetivo de restringir la cronología de los eventos individuales de movimientos en masa y su posible de correlación. Los resultados se integraron en esquemas cronoestratigráficos utilizando superficies de ruptura, relaciones transversales y de superposición de depósitos de deslizamiento y estratos posteriores para comprender los movimientos en masa en el contexto tectónico y temporal del entorno de la cuenca intermontana, así como para identificar los mecanismos desencadenantes de cada evento. El movimiento en masa MM-5 Guayllabamba es el resultado del colapso de la ladera suroeste del volcán Mojanda y fue desencadenado por la interacción de condiciones geológicas y morfológicas hace aproximadamente 0,81 Ma. El primer episodio de avalancha de escombros de los movimientos en masa MM-3 Oyacoto y MM-4 San Francisco podría estar relacionado con condiciones tanto geológicas como morfológicas, dadas las rocas altamente fracturadas y el levantamiento del anticlinal Bellavista-Catequilla que posteriormente fue inciso al pie de la ladera por la erosión fluvial. Este primer episodio de colapso probablemente ocurrió alrededor de los 0,8 Ma. El movimiento en masa MM-2 Batán posiblemente también fue desencadenado por una combinación de condiciones geológicas y morfológicas, asociadas a una reducción de los esfuerzos litostáticos que afectaron a las formaciones Chiche y Machángara y a un aumento de los esfuerzos de cizalla durante procesos de socavación fluvial lateral en los flancos de las áreas de origen. Esto apunta a un proceso vinculado entre la erosión fluvial y los procesos de levantamiento asociados a la evolución del anticlinal El Batán-La Bota que podría haber ocurrido entre 0,5 y 0,25 Ma. La voluminosa avalancha de escombros MM-1 Conocoto, así como el segundo episodio de avalancha de escombros que generó los movimientos en masa MM-3 Oyacoto y MM-4 San Francisco, fueron provocados por el colapso gravitacional de las formaciones Mojanda y Cangahua que se caracterizan por la intercalación de cenizas volcánicas. La falla del flanco oriental de los anticlinales probablemente estuvo asociada al incremento de la humedad disponible relacionada con las variaciones climáticas regionales del Holoceno. Los resultados de la cronología de los paleosuelos combinados con los datos cronoestratigráficos y paleoclimáticos regionales sugieren que estas avalanchas de escombros se desencadenaron entre 5 y 4 ka.
La tectónica activa ha modelado los rasgos morfológicos de la cuenca intermontana Quito-Guayllabamba. El desencadenamiento de movimientos en masa en este ambiente está asociado a rupturas en litologías del Pleistoceno (sedimentos lacustres, depósitos aluviales y volcánicos) sometidas a procesos de deformación, actividad sísmica y episodios superpuestos de variabilidad climática. El Distrito Metropolitano de Quito es parte integral de este complejo entorno y de las condiciones geológicas, climáticas y topográficas que continúan influyendo en el espacio geográfico urbano dentro de esta cuenca intermontana. La ciudad de Quito comprende el área de mayor consolidación urbana incluyendo las subcuencas de Quito y San Antonio, con una población de 2,872 millones de habitantes, lo que refleja la importancia del estudio de las amenazas geológicas y climáticas inherentes a esta región.
Arctic lakes located in permafrost regions are susceptible to catastrophic drainage. In this study, we reconstructed historical lake drainage events on the western Arctic Coastal Plain of Alaska between 1955 and 2017 using USGS topographic maps, historical aerial photography (1955), and Landsat Imagery (ca. 1975, ca. 2000, and annually since 2000). We identified 98 lakes larger than 10 ha that partially (>25% of area) or completely drained during the 62-year period. Decadal-scale lake drainage rates progressively declined from 2.0 lakes/yr (1955-1975), to 1.6 lakes/yr (1975-2000), and to 1.2 lakes/yr (2000-2017) in the ~30,000-km(2) study area. Detailed Landsat trend analysis between 2000 and 2017 identified two years, 2004 and 2006, with a cluster (five or more) of lake drainages probably associated with bank overtopping or headward erosion. To identify future potential lake drainages, we combined the historical lake drainage observations with a geospatial dataset describing lake elevation, hydrologic connectivity, and adjacent lake margin topographic gradients developed with a 5-m-resolution digital surface model. We identified ~1900 lakes likely to be prone to drainage in the future. Of the 20 lakes that drained in the most recent study period, 85% were identified in this future lake drainage potential dataset. Our assessment of historical lake drainage magnitude, mechanisms and pathways, and identification of potential future lake drainages provides insights into how arctic lowland landscapes may change and evolve in the coming decades to centuries.
Due to the high concentration of people and infrastructures in European cities, the possible impacts of climate change are particularly high (cities' social, economic and technical vulnerabilities). Adaptation measures to reduce the sensitivity of a city to climate risks are therefore of particular importance. Nevertheless, it is also common to develop compact and dense urban areas to reduce urban sprawl. Urban infill development and sustainable spatial climate policies are thus in apparent conflict with each other. This article examines how German cities deal with the tensions between these two policy fields. Using six case studies, a new heuristic analysis method is applied. This study identifies three key governance aspects that are essential for promoting the joint implementation: instruments, organisation and interaction. Based on our case studies, we conclude that successful implementation can only be achieved through integrative governance including all three domains.
The Central Andean region is characterized by diverse climate zones with sharp transitions between them. In this work, the area of interest is the South-Central Andes in northwestern Argentina that borders with Bolivia and Chile. The focus is the observation of soil moisture and water vapour with Global Navigation Satellite System (GNSS) remote-sensing methodologies. Because of the rapid temporal and spatial variations of water vapour and moisture circulations, monitoring this part of the hydrological cycle is crucial for understanding the mechanisms that control the local climate. Moreover, GNSS-based techniques have previously shown high potential and are appropriate for further investigation. This study includes both logistic-organization effort and data analysis. As for the prior, three GNSS ground stations were installed in remote locations in northwestern Argentina to acquire observations, where there was no availability of third-party data.
The methodological development for the observation of the climate variables of soil moisture and water vapour is independent and relies on different approaches. The soil-moisture estimation with GNSS reflectometry is an approximation that has demonstrated promising results, but it has yet to be operationally employed. Thus, a more advanced algorithm that exploits more observations from multiple satellite constellations was developed using data from two pilot stations in Germany. Additionally, this algorithm was slightly modified and used in a sea-level measurement campaign. Although the objective of this application is not related to monitoring hydrological parameters, its methodology is based on the same principles and helps to evaluate the core algorithm. On the other hand, water-vapour monitoring with GNSS observations is a well-established technique that is utilized operationally. Hence, the scope of this study is conducting a meteorological analysis by examining the along-the-zenith air-moisture levels and introducing indices related to the azimuthal gradient.
The results of the experiments indicate higher-quality soil moisture observations with the new algorithm. Furthermore, the analysis using the stations in northwestern Argentina illustrates the limits of this technology because of varying soil conditions and shows future research directions. The water-vapour analysis points out the strong influence of the topography on atmospheric moisture circulation and rainfall generation. Moreover, the GNSS time series allows for the identification of seasonal signatures, and the azimuthal-gradient indices permit the detection of main circulation pathways.
The hyperthermal events of the Cenozoic, including the Paleocene-Eocene Thermal Maximum, provide an opportunity to investigate the potential effects of climate warming on marine ecosystems. Here, we examine the shallow benthic marine communities preserved in the late Cretaceous to Eocene strata on the Gulf Coastal Plain (United States). In stark contrast to the ecological shifts following the end-Cretaceous mass extinction, our data show that the early Cenozoic hyperthermals did not have a long-term impact on the generic diversity nor composition of the Gulf Coastal Plain molluscan communities. We propose that these communities were resilient to climate change because molluscs are better adapted to high temperatures than other taxa, as demonstrated by their physiology and evolutionary history. In terms of resilience, these communities differ from other shallow-water carbonate ecosystems, such as reef communities, which record significant changes during the early Cenozoic hyperthermals. These data highlight the strikingly different responses of community types, i.e., the almost imperceptible response of molluscs versus the marked turnover of foraminifera and reef faunas. The impact on molluscan communities may have been low because detrimental conditions did not devastate the entire Gulf Coastal Plain, allowing molluscs to rapidly recolonise vacated areas once harsh environmental conditions ameliorated.
The origin of Asian monsoons
(2020)
The Cenozoic inception and development of the Asian monsoons remain unclear and have generated much debate, as several hypotheses regarding circulation patterns at work in Asia during the Eocene have been proposed in the few last decades. These include (a) the existence of modern-like monsoons since the early Eocene; (b) that of a weak South Asian monsoon (SAM) and little to no East Asian monsoon (EAM); or (c) a prevalence of the Intertropical Convergence Zone (ITCZ) migrations, also referred to as Indonesian-Australian monsoon (I-AM). As SAM and EAM are supposed to have been triggered or enhanced primarily by Asian palaeogeographic changes, their possible inception in the very dynamic Eocene palaeogeographic context remains an open question, both in the modelling and field-based communities. We investigate here Eocene Asian climate conditions using the IPSL-CM5A2 (Sepulchre et al., 2019) earth system model and revised palaeogeographies. Our Eocene climate simulation yields atmospheric circulation patterns in Asia substantially different from modern conditions. A large high-pressure area is simulated over the Tethys ocean, which generates intense low tropospheric winds blowing southward along the western flank of the proto-Himalayan-Tibetan plateau (HTP) system. This low-level wind system blocks, to latitudes lower than 10 degrees N, the migration of humid and warm air masses coming from the Indian Ocean. This strongly contrasts with the modern SAM, during which equatorial air masses reach a latitude of 20-25 degrees N over India and southeastern China. Another specific feature of our Eocene simulation is the widespread subsidence taking place over northern India in the midtroposphere (around 5000 m), preventing deep convective updraught that would transport water vapour up to the condensation level. Both processes lead to the onset of a broad arid region located over northern India and over the HTP. More humid regions of high seasonality in precipitation encircle this arid area, due to the prevalence of the Intertropical Convergence Zone (ITCZ) migrations (or Indonesian-Australian monsoon, I-AM) rather than monsoons. Although the existence of this central arid region may partly result from the specifics of our simulation (model dependence and palaeogeographic uncertainties) and has yet to be confirmed by proxy records, most of the observational evidence for Eocene monsoons are located in the highly seasonal transition zone between the arid area and the more humid surroundings. We thus suggest that a zonal arid climate prevailed over Asia before the initiation of monsoons that most likely occurred following Eocene palaeogeographic changes. Our results also show that precipitation seasonality should be used with caution to infer the presence of a monsoonal circulation and that the collection of new data in this arid area is of paramount importance to allow the debate to move forward.
Groundwater levels are monitored by environmental agencies to support the sustainable use of groundwater resources. For this purpose continuous and spatially comprehensive monitoring in high spatial and temporal resolution is desired. This leads to large datasets that have to be checked for quality and analysed to distinguish local anthropogenic influences from natural variability of the groundwater level dynamics at each well. Both technical problems with the measurements as well as local anthropogenic influences can lead to local anomalies in the hydrographs. We suggest a fast and efficient screening method for the identification of well-specific peculiarities in hydrographs of groundwater head monitoring networks. The only information required is a set of time series of groundwater heads all measured at the same instants of time. For each well of the monitoring network a reference hydrograph is calculated, describing expected “normal” behaviour at the respective well as is typical for the monitored region. The reference hydrograph is calculated by multiple linear regression of the observed hydrograph with the “stable” principal components (PCs) of a principal component analysis of all groundwater head series of the network as predictor variables. The stable PCs are those PCs which were found in a random subsampling procedure to be rather insensitive to the specific selection of the analysed observation wells, i.e. complete series, and to the specific selection of measurement dates. Hence they can be considered to be representative for the monitored region in the respective period. The residuals of the reference hydrograph describe local deviations from the normal behaviour. Peculiarities in the residuals allow the data to be checked for measurement errors and the wells with a possible anthropogenic influence to be identified. The approach was tested with 141 groundwater head time series from the state authority groundwater monitoring network in northeastern Germany covering the period from 1993 to 2013 at an approximately weekly frequency of measurement.
New Zealand's Alpine Fault is a large, platebounding strike-slip fault, which ruptures in large (M-w > 8) earthquakes. We conducted field and laboratory analyses of fault rocks to assess its fault zone architecture. Results reveal that the Alpine Fault Zone has a complex geometry, comprising an anastomosing network of multiple slip planes that have accommodated different amounts of displacement. This contrasts with the previous perception of the Alpine Fault Zone, which assumes a single principal slip zone accommodated all displacement. This interpretation is supported by results of drilling projects and geophysical investigations. Furthermore, observations presented here show that the young, largely unconsolidated sediments that constitute the footwall at shallow depths have a significant influence on fault gouge rheological properties and structure.