Refine
Year of publication
- 2016 (291) (remove)
Document Type
- Article (221)
- Doctoral Thesis (37)
- Other (14)
- Postprint (12)
- Review (5)
- Habilitation Thesis (1)
- Report (1)
Is part of the Bibliography
- yes (291) (remove)
Keywords
- climate change (5)
- erosion (5)
- water balance (5)
- Pollen (4)
- August 2002 flood (3)
- Body waves (3)
- Central Europe (3)
- Floods Directive (3)
- Himalaya (3)
- Himalayas (3)
- Inversion (3)
- June 2013 flood (3)
- earthquake (3)
- geomorphology (3)
- glacial hazards (3)
- glacial lake outburst floods (3)
- governance (3)
- hydropower (3)
- risk management cycle (3)
- soil moisture (3)
- thermochronology (3)
- water resources (3)
- Anatolia (2)
- Aral Sea (2)
- Arctic (2)
- Barasona Reservoir (2)
- Barents Sea (2)
- Bodenfeuchte (2)
- Central Andes (2)
- Central Asia (2)
- Climate (2)
- Climate change (2)
- Coastal erosion (2)
- Complex networks (2)
- Compression (2)
- Diatoms (2)
- Drought (2)
- Earthquake source observations (2)
- Ebro basin (2)
- Eclogite (2)
- Equatorial Pacific (2)
- Equatorial plasma irregularities (2)
- Erdbeben (2)
- Erosion (2)
- Flooding (2)
- GLDAS (2)
- GRACE (2)
- Gas diffusion layer (2)
- Geochronology (2)
- Geologie (2)
- Geomorphologie (2)
- Gulf of Mexico (2)
- High-pressure metamorphism (2)
- Holocene (2)
- Hydrologie (2)
- Hydrus-2D (2)
- Klimawandel (2)
- Lake Mead (2)
- Lake Van (2)
- Larix gmelinii (2)
- Last Glacial Maximum (2)
- Lateglacial (2)
- LiDAR (2)
- Neotektonik (2)
- Neotethys (2)
- Nitrogen (2)
- Raman spectroscopy (2)
- Sampling (2)
- Seismicity and tectonics (2)
- South America (2)
- Swarm constellation (2)
- Theoretical seismology (2)
- Thermochronologie (2)
- Throughfall (2)
- UAV (2)
- VI (2)
- WGHM (2)
- X-ray absorption (2)
- adaption measure (2)
- agriculture (2)
- carbon export (2)
- climate (2)
- climate extremes (2)
- coastal wetland (2)
- cosmogenic nuclides (2)
- deep biosphere (2)
- dendrometer measurements (2)
- ditch irrigation (2)
- drainage of the catchment area (2)
- evapotranspiration (2)
- event coincidence analysis (2)
- floods (2)
- geology (2)
- groundwater flow (2)
- groundwater level (2)
- groundwater surface water interaction (2)
- growth response (2)
- hydrogenase (2)
- hydrology (2)
- imaging spectroscopy (2)
- landslide (2)
- landslides (2)
- management effects (2)
- microbial activity (2)
- mitigation (2)
- multispectral (2)
- neotectonics (2)
- remote sensing (2)
- required minimum runoff (2)
- reservoir (2)
- soil landscape (2)
- subduction zone (2)
- system analysis (2)
- tectonics (2)
- thermische Modellierung (2)
- tritium assay (2)
- water balance model (2)
- water budget (2)
- water fluxes (2)
- wetland (2)
- 0 (1)
- 10-Be terrestrial cosmogenic nuclides (1)
- ALS (1)
- AMSR-E (1)
- AMSR2 (1)
- ANN (1)
- AVHRR (1)
- Acanthocyclops (1)
- Active seismic (1)
- Adana Basin (1)
- Adaptation to climate change (1)
- Adaptive value (1)
- Aegean (1)
- Afyon zone (1)
- Agricultural fields (1)
- Agricultural landscape (1)
- Airborne laser scanning (ALS) (1)
- Alanya (1)
- Altai (1)
- Amides (1)
- Amoebal silicon (1)
- Amplitude ratio (1)
- Anatolide-Tauride Block (1)
- Anisotropy (1)
- Apatit-(U-Th)/He Datierung (1)
- Apatit-Spaltspurendatierung (1)
- Apatite (U-Th)/He, apatite fission track dating (1)
- Aquatic and terrestrial ecosystems (1)
- Ar-40/Ar-39 (1)
- Ar-40/Ar-39 laser ablation (1)
- Archean (1)
- Arctic limnology (1)
- Autocorrelation (1)
- Aymara (1)
- Baltic Sea (1)
- Baltic Sea Coast (1)
- Barasona reservoir (1)
- Barberton Greenstone Belt (1)
- Basilika formation (1)
- Bayesian classification (1)
- Bayesian inference (1)
- Beckenentwicklung (1)
- Beckenstruktur (1)
- Beringia (1)
- Biogenic silica (1)
- Biomarker (1)
- Biosilicification (1)
- Blueschist (1)
- Bodenheterogenität (1)
- Bodenhydrologie (1)
- Bolboschoenus maritimus (1)
- Borehole image logs (1)
- Brazil (1)
- Bryophytes (1)
- Buntsandstein (1)
- C-14 (1)
- C-14 analyses (1)
- C3 and C4 grasses (1)
- Caatinga (1)
- Campanian-Maastrichtian boundary (1)
- Can Tho (1)
- Canary Islands (1)
- Carbon (1)
- Carbon cycle (1)
- Carbon redistribution (1)
- Carboniferous magmatism (1)
- Catchment scale (1)
- Central Tertiary Basin (1)
- Chaiten volcano (1)
- Changbai mountains (1)
- Changes in fluvial systems (1)
- Characteristic pollen source area (1)
- Chile (1)
- City boundaries (1)
- Cladocera (1)
- Cladocoropsis (1)
- Climate variability (1)
- Closure temperature (1)
- Coda waves (1)
- Comets (1)
- Comparative study (1)
- Compound-specific carbon isotope (1)
- Computational seismology (1)
- Computed tomography (1)
- Concentration-discharge relationship (1)
- Concept (1)
- Confidence interval (1)
- Consumption (1)
- Continuity (1)
- Controlled source seismology (1)
- Cosmogenic Be-10 exposure dating (1)
- Cristobalite (1)
- Cryolithology (1)
- Cultural ecosystem services (1)
- Culture growth dynamics (1)
- DFT (1)
- DOC vs. DIC (1)
- Dairy cow (1)
- Damage modeling (1)
- Decomposition (1)
- Deep fluids (1)
- Deglaciation (1)
- Degradation (1)
- Desert wetland ecosystems (1)
- Desertification (1)
- Deuterium excess (1)
- Diatom frustule (1)
- Dispersion curve (1)
- Dispersion curves (1)
- Dispersionskurven (1)
- Distachyapites (1)
- Diurnal fluctuations (1)
- Dominant link directions (1)
- Drainage capture (1)
- Drinking water quality (1)
- Dynamics: seismotectonics (1)
- EDX (1)
- EXAFS (1)
- Early Eocene (1)
- Earth materials (1)
- Earthworms (1)
- East African Rift (1)
- East African Rift System (1)
- East African rift system (1)
- East Asian summer monsoon (1)
- Eastern Alps (1)
- Ecosystem research (1)
- Ecosystem services (1)
- Education (1)
- Effective dimensionality (1)
- Eifel Depression (1)
- Eifeler Nord-Süd-Zone (1)
- Eisdamm (1)
- Eismodell (1)
- El Hierro (1)
- Elbe (1)
- Elbe estuary (1)
- Elbe Ästuar (1)
- Electrical conductivity (1)
- Electrical resistivity imaging (1)
- EnGeoMAP 2 (1)
- EnMAP (1)
- Enhanced Geothermal Systems (1)
- Eocene (1)
- Ephedripites (1)
- Epiphytic foraminifera (1)
- Equilibrium phase modeling (1)
- Erdbeeben (1)
- Erdrutsch (1)
- Eroded soil types (1)
- Eruptive recurrence (1)
- Euglyphida (1)
- Europa (1)
- Europe (1)
- European Alps (1)
- European beech forest (1)
- Europäische Alpen (1)
- Evaporites (1)
- Evapotranspiration (1)
- Event synchronization (1)
- Expectation maximisation (1)
- Export regime (1)
- Expositionsaltersdatierung (1)
- Extent (1)
- Extreme rainfall (1)
- Extremniederschlag (1)
- Fen stratigraphy (1)
- Fennoscandian Ice Sheet (1)
- First ovulation (1)
- Flash floods (1)
- Flood generating processes (1)
- Flood risk (1)
- Flow regime (1)
- Fluid (1)
- Forest change (1)
- Forest mineral topsoil (1)
- Full-waveform (1)
- GNSS (1)
- GPM (1)
- Gabbro (1)
- Gebäudenergiebedarf (1)
- Geochemie (1)
- Geophysical methods (1)
- Geostatistics (1)
- Geothermal water (1)
- Geothermie (1)
- Geoökologie (1)
- Glacial geomorphology (1)
- Glaciation (1)
- Glaucophane (1)
- Glazialisostasie (1)
- Gnetaceaepollenites (1)
- Gondwana (1)
- Grain-size (1)
- Granitoid magmas (1)
- Ground penetrating radar (1)
- Ground-motion prediction equation (1)
- Groundwater (1)
- Grundgesteinshöhe (1)
- Gypsum (1)
- Gyttja (1)
- H/V ratio technique (1)
- Hangrutsch (1)
- Hangrutschungen (1)
- Haushalte (1)
- Hazard (1)
- Hepatic enzyme (1)
- Hf isotopes (1)
- Hierarchical model (1)
- High Arctic Large Igneous Province (1)
- High rate GPS (1)
- Hillslope pedosequence (1)
- Himalaja (1)
- Hochwasser (1)
- Hochwasserrisikoanalysen (1)
- Hochwasserrisikokette (1)
- Hochwassertypen (1)
- Holocene Thermal Maximum (1)
- Holozän (1)
- Humahuaca Basin (1)
- Hydroclimate (1)
- Hydrological monitoring (1)
- Hydrolysis (1)
- Hydrophobic treatment (1)
- Hydrus-1D (1)
- Hyperion (1)
- Hyporheic zone (1)
- IBM (1)
- Iberian Peninsula (1)
- Ice model (1)
- Ice sheet dynamics (1)
- Ice-wedge polygon (1)
- Iceland (1)
- In-situ cosmogenic Be-10 (1)
- In-stream geomorphological structures (1)
- In-stream processes (1)
- InSAR (1)
- InSAR- Techniken (1)
- Index of dispersion (1)
- Indian Summer Monsoon (1)
- Indian monsoon (1)
- Indicator species (1)
- Indus (1)
- Inflow and outflow (1)
- Infrared observations (1)
- Infrared spectroscopy (1)
- Initial ecosystem (1)
- Interferometrie (1)
- Interferometry (1)
- Interior Alaska (1)
- Interzeptionsverdunstung (1)
- Inundation (1)
- Inversionstheorie (1)
- Ionospheric scale lengths (1)
- Island (1)
- Isochrones (1)
- Jwalamukhi Thrust (1)
- K-means technique (1)
- Karakoram (1)
- Karakorum (1)
- Kernel occurrence rate (1)
- Kettle hole (1)
- Kinetics (1)
- Klimavariabilität (1)
- Kohlenstoffkreislauf (1)
- Kokchetavite (1)
- Kumdykolite (1)
- Küstenlinien (1)
- LAI (1)
- LGM (1)
- Lake Towuti (1)
- Lake-ice cover (1)
- Landsat 8 (1)
- Landscape aesthetics (1)
- Landscape dynamics (1)
- Landscape preferences (1)
- Landscape values (1)
- Landschaftsentwicklung (1)
- Larger benthic foraminifera (1)
- Late Cretaceous (1)
- Lateinamerika (1)
- Latin America (1)
- Lech catchment (1)
- Lena Delta (1)
- Level of confidence (1)
- Lipid biomarker (1)
- Lipids (1)
- Liquid water distribution (1)
- Literature review (1)
- Liver function (1)
- Livestock (1)
- Loess (1)
- Low-centred polygon (1)
- Lower Devonian (1)
- Lower Paleolithic (1)
- Lowland catchment (1)
- Luxembourg (1)
- Luxemburg (1)
- Lysimeter control systems (1)
- MARS (1)
- MASW (1)
- MAT(mr) paleothermometer (1)
- MODIS (1)
- Malagasy/Kuunga orogeny (1)
- Management (1)
- Mantelplumes (1)
- Marine Isotope Stage 13 (1)
- Mass balance approach (1)
- Maximum magnitude of earthquake (1)
- Mean July temperature (1)
- Mediterranean (1)
- Mediterranean fluvial systems (1)
- Mediterranean shallow lake (1)
- Meerfelder Maar (1)
- Mekong Delta (1)
- Menderes Massif (1)
- Mesozoic (1)
- Mesozoikum (1)
- Messinian Erosional Surface (1)
- Messinian Salinity Crisis (1)
- Meta-plagiogranite (1)
- Metamorphism (1)
- Meteorites (1)
- Mg/Ca (1)
- Micro-aggregates (1)
- Microscopy (1)
- Microtremors (1)
- Mid-late Holocene (1)
- Mixed coniferous and deciduous broad-leaved woodland (1)
- Modern analogue technique (1)
- Molecular design (1)
- Monetary valuation (1)
- Monitoring (1)
- Moodies Group (1)
- Mountain hydrology (1)
- Muster der Bodenfeuchte (1)
- NE Spain (1)
- NMDS (1)
- NW-Argentine Andes (1)
- Na-pyrophosphate soluble organic matter (1)
- Namche Barwa (1)
- Nanogranites (1)
- Naturgefahren (1)
- Neutronen (1)
- New Zealand (1)
- Nitrate (1)
- Nitrate retention (1)
- Non-ergodic PSHA (1)
- Non-monetary valuation (1)
- Normal fault evolution (1)
- North Atlantic Large Igneous Province (1)
- Nährstoffeinträge (1)
- ODD model description (1)
- Oberflächenwärmefluss (1)
- Oceanic transform and fracture zone processes (1)
- Oman (1)
- Omphacite (1)
- Optically stimulated luminescence (1)
- Ordination (1)
- Organic carbon (1)
- Organic chemistry (1)
- Organic matter (1)
- Organic matter stabilization (1)
- Orogen-parallel lateral extrusion (1)
- Orthotropy (1)
- Ostafrikansches Rift (1)
- Ostracoda (1)
- Oyster (1)
- Palaeoclimate (1)
- Palaeogene (1)
- Paleoecology (1)
- Paleoenvironment (1)
- Paleogene (1)
- Paleosol (1)
- Paleotethys (1)
- Palynology (1)
- Paläoklima (1)
- Paläolimnologie (1)
- Pamir-Tien Shan (1)
- Panjal Traps (1)
- Paris Basin (1)
- Paris-Edinburgh press (1)
- Pariser Becken (1)
- Partial melt (1)
- Particle-size fractions (1)
- Passive Microwave (1)
- Passive seismic (1)
- Patagonia (1)
- Peak flow trends (1)
- Peak-over-threshold (1)
- Peat (1)
- Peat properties (1)
- Perm (1)
- Permafrost (1)
- Permafrost coasts (1)
- Permafrost ecosystem (1)
- Permafrost peatlands (1)
- Permafrostdegradation (1)
- Permian (1)
- Peruvian fore arc (1)
- Petrologie (1)
- Pflanzenwachs (1)
- Pflanzenwasserzustand (1)
- Pflaume (1)
- Phosphorus (1)
- Pigments (1)
- Plant macrofossils (1)
- Plant n-alkanes (1)
- Point cloud (1)
- Polymerization (1)
- Polymorphs (1)
- Population density (1)
- Pore network modeling (1)
- Posterior estimation (1)
- Precipitation events (1)
- Procrustes rotation (1)
- Präzision Gartenbau (1)
- Puna Plateau (1)
- Pyrenees (1)
- Quantitative reconstruction (1)
- Quarter-wavelength principle (1)
- Quelle Inversion (1)
- Radiocarbon (1)
- Rainfall (1)
- Rainfall floods (1)
- Rapid exhumation/cooling (1)
- Rayleigh waves (1)
- Real time (1)
- Reference station (1)
- Regional climate models (1)
- Regionalization (1)
- Reproductive performance (1)
- Reservoir (1)
- Reservoir temperature (1)
- Reservoirs (1)
- Residual maximum likelihood (1)
- Respiration rate (1)
- Response function (1)
- Rewetting (1)
- Rhenohercynian Zone (1)
- Rhenohercynische Zone (1)
- Riparian vegetation (1)
- River Esera (1)
- River restoration (1)
- River-groundwater exchange (1)
- Root water uptake (1)
- Rooting depth (1)
- Rossby waves (1)
- Rover station (1)
- Runoff modeling (1)
- Russia (1)
- Röntgenabsorptionspektroskopie (1)
- Rückenkollision (1)
- SH waves (1)
- SRTM improvements (1)
- SSMI/S (1)
- SWAT (1)
- Sanabria Lake (1)
- Sanierung (1)
- Sarmentofascis (1)
- Satelliten-Fernerkundung (1)
- Scenarios (1)
- Schadensabschätzung (1)
- Sclerochronology (1)
- Scotland (1)
- Seagrasses (1)
- Seawater intrusion (1)
- Sectoral emissions (1)
- Sediment (1)
- Sediment distribution (1)
- Sediment geochemistry (1)
- Sediment load (1)
- Sedimentmächtigkeit (1)
- Sedimentvolumen (1)
- Seeausbrüche (1)
- Seesediment (1)
- Seismic anisotropy (1)
- Seismic attenuation (1)
- Seismic tomography (1)
- Seismicity (1)
- Self-organizing map (1)
- Semi-arid (1)
- Sentinel-2 MSI (1)
- Shyok Fluss (1)
- Shyok River (1)
- SiO(2)Molecular dynamics (1)
- SiO2-H2O (1)
- Siberia (1)
- Silk Road (1)
- Simulation (1)
- Sinkholes (1)
- Site characterization (1)
- Siurana Reservoir (1)
- Slab break-off (1)
- Slab roll-back (1)
- Snow-Water Equivalent (1)
- Snowmelt floods (1)
- Social valuation (1)
- Soil (1)
- Soil C leaching (1)
- Soil deposition (1)
- Soil erosion (1)
- Soil tillage (1)
- Soil water balance simulation (1)
- Sommer et al. 2006 (1)
- South American Monsoon System (1)
- South American monsoon system (1)
- South Central Andes (1)
- South Eifel (1)
- Spatial distribution (1)
- Spectrophotometry (1)
- Sponge spicule (1)
- Sponges (1)
- Spreewald wetland (1)
- Spurenelementverteilung (1)
- Stable water isotopes (1)
- Stalagmite (1)
- Standorteffekte (1)
- Statistical downscaling (1)
- Statistical seismology (1)
- Stream network (1)
- Stress field (1)
- Stress pattern (1)
- Stromsektor (1)
- Strong motion (1)
- Strontium isotope stratigraphy (1)
- Structural inheritance (1)
- Sturzflut (1)
- Subduction (1)
- Subduktionszone (1)
- Sulfate (1)
- Sulfatreduktion (1)
- Summer and winter temperature (1)
- Surface-wave methods (1)
- Suspended sediment (1)
- Suspended sediment transport (1)
- Sutlej River (1)
- Svalbard (1)
- Synchronization (1)
- Synchrotron X-ray (1)
- Synchrotron tomography (1)
- Syntaxe (1)
- Synthetic Aperture Radar (1)
- Syria (1)
- Systematics (1)
- Südeifel (1)
- TRMM (1)
- Talik (1)
- Tananao Complex (1)
- Taranaki Basin (1)
- Tauride (1)
- Taurus petroleum system (1)
- Tektonik (1)
- Temperature time series (1)
- Temporal clustering (1)
- Temporal dynamics (1)
- Temporary pond (1)
- Terrestrial C sink (1)
- Terrestrial Si cycle (1)
- Testate amoeba shell (1)
- Thermo-sensitive tracers (1)
- Thermokarst (1)
- Thermokarstprozesse (1)
- Tibet Plateau (1)
- Tibetan Plateau (1)
- Tiefenversickerung (1)
- Tiefer See (1)
- Tien Shan (1)
- Time-lag effects (1)
- Time-series analysis (1)
- Topographie (1)
- Trace element geochemistry (1)
- Trace elements (1)
- Transbaikalia (1)
- Transfer function (1)
- Transformation hydrologischer Signale (1)
- Transhimalaya (1)
- Tree line (1)
- Tremp basin (1)
- Trier-Luxembourg Basin (1)
- Trier-Luxembourg Embayment (1)
- Trier-Luxemburger Becken (1)
- Trier-Luxemburger Bucht (1)
- Tropical forest (1)
- Tropics (1)
- Tso Moriri Lake (1)
- Tsunami-Frühwarnsystem (1)
- Tundra (1)
- Tundra-taiga ecotone (1)
- Turkey (1)
- UHP edogites and felsic gneisses (1)
- UNESCO (1)
- Umweltrekonstruktion (1)
- Ungauged catchments (1)
- Unterdevon (1)
- Upper Cretaceous (1)
- Urban energy (1)
- Urban sprawl (1)
- V-s profiles (1)
- V-s,V-30 (1)
- Valley fill (1)
- Vascular plants (1)
- Vegetation (1)
- Verschüttungsaltersdatierung (1)
- Vertical pollen dispersal and deposition (1)
- Vietnam (1)
- Virtual active seismic (1)
- Visualization (1)
- Volcanic disturbances (1)
- Vs Profile (1)
- Vs profiles (1)
- Vulnerability (1)
- Vulnerability mapping (1)
- WA-PLS (1)
- Wall paintings (1)
- Wasser-Monitoring (1)
- Wasserhaushalt (1)
- Water (1)
- Water balance (1)
- Water quality (1)
- Water storage (1)
- Water transport (1)
- Wave propagation (1)
- Wavelet power spectrum (1)
- Weather radar (1)
- Weilerbach-Mulde (1)
- Wetterlagen (1)
- Wittlicher Senke (1)
- Woody coverage (1)
- Wärmeleitfähigkeit (1)
- X-ray Raman scattering (1)
- X-ray fluorescence (1)
- XRF (1)
- Yarlung-Tsangpo Gorge (1)
- Yarlung-Tsangpo Schlucht (1)
- Yuli belt (1)
- Zanskar (1)
- Zeitreihenanalyse (1)
- Zentralanden (1)
- Zircon U-Pb age (1)
- active seismic (1)
- aeolian (1)
- aktive Seismik (1)
- alluvial-fan sedimentation (1)
- antecedent conditions (1)
- apatite fission-track thermochronology (1)
- apatite helium thermochronology (1)
- aquatic ecosystems (1)
- aquatischen Ökosystemen (1)
- arctic water bodies (1)
- arktische Gewässer (1)
- artificial neural networks (1)
- asthenospheric slab-window (1)
- asthenospherisches "slab-window" (1)
- asymmetric pair distribution function (1)
- attenuation (1)
- attitudinal transects (1)
- basin analysis (1)
- basin evolution (1)
- basin structure (1)
- bedrock elevation (1)
- bentonite (1)
- berylium-10 (1)
- bioindicators (1)
- biomanipulation (1)
- biomarker (1)
- biomaterial (1)
- biomineralization (1)
- biosynthetic fractionation (1)
- bonding transition (1)
- bottom waters (1)
- brackish marsh (1)
- branched GDGTs (1)
- brushite (1)
- burial dating (1)
- calcium phosphate (1)
- capacitive sensors (1)
- carbon cycle (1)
- carbon cycling (1)
- carbon fluxes (1)
- carbonatites (1)
- cartography (1)
- cellulose (1)
- central-eastern Beringia (1)
- cirrus detection (1)
- climate instability (1)
- climate variability (1)
- cloud detection (1)
- connectivity (1)
- convective rainfall (1)
- coordination transformation (1)
- coregistration (1)
- cosmic rays (1)
- cosmogenic radionuclide-based dating (1)
- critical meteorological condition (1)
- crustal anatexis (1)
- cryostratigraphy (1)
- damage (1)
- damage assessment (1)
- decision trees (1)
- deep seepage (1)
- density-functional theory (1)
- deuterium (1)
- diamond anvil cell (1)
- digital elevation model (1)
- direct georeferencing (1)
- dispersion curves (1)
- dynamic topography (1)
- early warning (1)
- eastern Mediterranean (1)
- ecological indication (1)
- electronic structure (1)
- emergency response (1)
- energy demand (1)
- environmental reconstruction (1)
- environmental remediation (1)
- experimental design (1)
- exposure age dating (1)
- extracellular DNA (1)
- extreme events (1)
- extreme hydro-meteorologische Ereignisse (1)
- extreme hydrometeorological events (1)
- extreme precipitation (1)
- fallout radionuclides (1)
- fault linkage (1)
- fens (1)
- flash flood (1)
- flood damage (1)
- flood loss (1)
- flood risk (1)
- flood risk analysis (1)
- flood risk management (1)
- flood types (1)
- floodplain inundation (1)
- flow velocity (1)
- fluvial (1)
- fluvial terrace (1)
- fluvial terraces (1)
- frequency analysis (1)
- freshwater ostracods (1)
- garnet (1)
- geoecology (1)
- geothermal energy (1)
- glacial incision (1)
- glacial isostatic adjustment (1)
- glasses (1)
- glaziale Einschneidung (1)
- global navigation satellite systems (1)
- hafnium analysis (1)
- hafnon (1)
- heavy metals (1)
- heavy rainfall (1)
- heterogeneity in soil hydraulic properties (1)
- high pressure and temperature (1)
- high pressure research (1)
- high temporal resolution (1)
- human impact (1)
- human-environment system (1)
- hydraulic conductivity (1)
- hydraulic simulation (1)
- hydrogen stable isotopes (1)
- hydrologische Vorbedingungen (1)
- hydrothermal systems (1)
- hydrothermale Systeme (1)
- hydroyxapatite (1)
- ice dam (1)
- immobilization (1)
- impoundment rate (1)
- in situ stress (1)
- indigenous people (1)
- inelastic X-ray scattering (1)
- interception (1)
- interferometry (1)
- intermontane Talverfüllungen (1)
- intermontane valley fill (1)
- invasive species (1)
- inverse theory (1)
- inversion (1)
- ionospheric scale lengths (1)
- iron reduction (1)
- iron-rich sediment (1)
- irrigation runoff (1)
- isostatic uplift (1)
- isostatische Hebung (1)
- isotopes (1)
- kontinuierlicher Simulationsansatz (1)
- kosmische Strahlung (1)
- kosmogene Nuklide (1)
- kosmogene Radionuklid-basierte Datierung (1)
- künstliche neurale Netzwerke (1)
- lacustrine primary productivity (LPP) (1)
- lake sediment (1)
- land restoration; NDVI (1)
- landscape connectivity (1)
- landscape evolution (1)
- late Quaternary (1)
- leaf water evaporative H-2-enrichment (1)
- leaf wax delta D (1)
- leaf wax n-alkanes (1)
- leaf-wax n-alkane delta D (1)
- liquid structure (1)
- local structure (1)
- lokale Struktur (1)
- machine learning (1)
- mantle plume (1)
- mantle plumes (1)
- marine Terrassen (1)
- marine terraces (1)
- mass wasting (1)
- mechanical pressure (1)
- melt inclusions (1)
- melt inclusions; nanocarbonatites (1)
- melts (1)
- menschliche Einflüsse (1)
- microbial methane oxidation (1)
- mid-latitudes flow (1)
- mikrobielle aerobe Methanoxidation (1)
- mineral mapping (1)
- minerals (1)
- mire (1)
- monsoon (1)
- morphological adaptation (1)
- mountains near cities (1)
- multiparameter (1)
- multisensor (1)
- multiyear drought (1)
- n-Alkanes (1)
- nanogranite (1)
- nanogranites (1)
- natural hazard management (1)
- natural hazards (1)
- neutrons (1)
- normal-fault evolution (1)
- numerical modelling (1)
- numerical models (1)
- numerische Modellierung (1)
- nutrient emissions (1)
- oceanic lithosphere (1)
- optically stimulated luminescence (1)
- oroclinal bending (1)
- orogenic processes (1)
- orogenic wedge (1)
- orographic barrier uplift (1)
- outburst floods (1)
- oxidation state (1)
- palaeoclimate (1)
- palaeoenvironmental reconstruction (1)
- paleo-erosion rate (1)
- paleoaltimetry (1)
- paleoaltimetry proxies (1)
- paleolimnology (1)
- parametric georeferencing (1)
- partial melting (1)
- particle size (1)
- passive Seismik (1)
- passive seismic (1)
- patched vegetation cover (1)
- patterned ground (1)
- perception (1)
- periglacial landscape evolution (1)
- periglaziale Landschaftsentwicklung (1)
- peritectic phase (1)
- permafrost (1)
- permafrost degradation (1)
- permanent deformation (1)
- permanente Verformung (1)
- petrology (1)
- petrothermal systems (1)
- petrothermale Systeme (1)
- phenotypic plasticity (1)
- physical stratigraphy (1)
- pioneer zone (1)
- plant wax biomarker (1)
- plant waxes (1)
- plate tectonics (1)
- plum (1)
- pluvial floods (1)
- pollen accumulation rates (1)
- pollen morphology (1)
- polyamine (1)
- polyammonium salt (1)
- polycarboxylate (1)
- polyzwitterion (1)
- precipitation (1)
- precision horticulture (1)
- preferences in land management (1)
- preparedness (1)
- preprocessing (1)
- probabilistic (1)
- quantitative precipitation estimation (1)
- radiogene Wärmeproduktion (1)
- radiogenic heat production (1)
- railway transportation (1)
- rainfall (1)
- rainfall-runoff (1)
- ray tracing (1)
- regional deformation (1)
- remotely sensed evapotranspiration (1)
- residential buildings (1)
- ridge-collision (1)
- rigorous geocoding (1)
- risk model chain (1)
- root system (1)
- run-on (1)
- räumliche Variabilität (1)
- saline Seen (1)
- saline lakes (1)
- scaling (1)
- sediment delivery processes (1)
- sediment source fingerprinting (1)
- sediment thickness (1)
- sediment volume (1)
- sedimentary microbes (1)
- seismic source inversion (1)
- semi-arid (1)
- sensor alignment (1)
- sensor fusion (1)
- shadow detection (1)
- shorelines (1)
- shortening (1)
- simulation on a day-to-day-basis (1)
- site effects (1)
- snow detection (1)
- social valuation (1)
- soil heterogeneity (1)
- soil hydrology (1)
- soil moisture dynamics (1)
- soil moisture patterns (1)
- solid solution (1)
- spatial variability (1)
- spin transition (1)
- stabile Isotope (1)
- stable isotopes (1)
- steepness index (1)
- subduction initiation (1)
- sulfate reduction (1)
- sulphate reduction (1)
- surface heat flow (1)
- surface sealing (1)
- surface water flooding (1)
- susceptibility of the European electricity sector (1)
- syntaxis (1)
- synthesis (1)
- tagesaktuelle Simulation (1)
- tectonic geomorphology (1)
- tectonic uplift (1)
- tektonische Geomorphologie (1)
- tektonische Hebung (1)
- tephra (1)
- terrestrial cosmogenic nuclides (1)
- thermal conductivity (1)
- thermal modeling (1)
- thermal modelling (1)
- thermodynamic modelling (1)
- thermodynamische Modellierungen (1)
- thermokarst lake dynamics (1)
- thermokarst processes (1)
- thick-skinned deformation (1)
- time series analysis (1)
- topography (1)
- trace elements (1)
- transformation of hydrological signals (1)
- tree water status (1)
- trench-parallel extension (1)
- tsunami early warning (1)
- uncertainty (1)
- urban green spaces (1)
- validation (1)
- variogram (1)
- varved lake sediments (1)
- vegetation (1)
- vegetation change (1)
- virtual active seismic (1)
- virtuelle aktive Seismik (1)
- visualisation (1)
- volcanic glass (1)
- warvierte Seesedimente (1)
- water demand (1)
- water management (1)
- water monitoring (1)
- water-limited environment (1)
- weather patterns (1)
- wet meadow (1)
- whole Earth images (1)
- wildfire (1)
- x-ray absorption spectroscopy (1)
- yedoma (1)
- zentral-östliches Beringia (1)
- zircon (1)
- zircon U-Pb geochronology (1)
- zircon provenance (1)
- Überschwemmungsflächen (1)
Institute
- Institut für Geowissenschaften (291) (remove)
The problem of estimating the maximum possible earthquake magnitude m(max) has attracted growing attention in recent years. Due to sparse data, the role of uncertainties becomes crucial. In this work, we determine the uncertainties related to the maximum magnitude in terms of confidence intervals. Using an earthquake catalog of Iran, m(max) is estimated for different predefined levels of confidence in six seismotectonic zones. Assuming the doubly truncated Gutenberg-Richter distribution as a statistical model for earthquake magnitudes, confidence intervals for the maximum possible magnitude of earthquakes are calculated in each zone. While the lower limit of the confidence interval is the magnitude of the maximum observed event, the upper limit is calculated from the catalog and the statistical model. For this aim, we use the original catalog which no declustering methods applied on as well as a declustered version of the catalog. Based on the study by Holschneider et al. (Bull Seismol Soc Am 101(4): 1649-1659, 2011), the confidence interval for m(max) is frequently unbounded, especially if high levels of confidence are required. In this case, no information is gained from the data. Therefore, we elaborate for which settings finite confidence levels are obtained. In this work, Iran is divided into six seismotectonic zones, namely Alborz, Azerbaijan, Zagros, Makran, Kopet Dagh, Central Iran. Although calculations of the confidence interval in Central Iran and Zagros seismotectonic zones are relatively acceptable for meaningful levels of confidence, results in Kopet Dagh, Alborz, Azerbaijan and Makran are not that much promising. The results indicate that estimating mmax from an earthquake catalog for reasonable levels of confidence alone is almost impossible.
Flood loss modeling is an important component for risk analyses and decision support in flood risk management. Commonly, flood loss models describe complex damaging processes by simple, deterministic approaches like depth-damage functions and are associated with large uncertainty. To improve flood loss estimation and to provide quantitative information about the uncertainty associated with loss modeling, a probabilistic, multivariable Bagging decision Tree Flood Loss Estimation MOdel (BT-FLEMO) for residential buildings was developed. The application of BT-FLEMO provides a probability distribution of estimated losses to residential buildings per municipality. BT-FLEMO was applied and validated at the mesoscale in 19 municipalities that were affected during the 2002 flood by the River Mulde in Saxony, Germany. Validation was undertaken on the one hand via a comparison with six deterministic loss models, including both depth-damage functions and multivariable models. On the other hand, the results were compared with official loss data. BT-FLEMO outperforms deterministic, univariable, and multivariable models with regard to model accuracy, although the prediction uncertainty remains high. An important advantage of BT-FLEMO is the quantification of prediction uncertainty. The probability distribution of loss estimates by BT-FLEMO well represents the variation range of loss estimates of the other models in the case study.
In this study, we investigated the scale sizes of equatorial plasma irregularities (EPIs) using measurements from the Swarm satellites during its early mission and final constellation phases. We found that with longitudinal separation between Swarm satellites larger than 0.4°, no significant correlation was found any more. This result suggests that EPI structures include plasma density scale sizes less than 44 km in the zonal direction. During the Swarm earlier mission phase, clearly better EPI correlations are obtained in the northern hemisphere, implying more fragmented irregularities in the southern hemisphere where the ambient magnetic field is low. The previously reported inverted-C shell structure of EPIs is generally confirmed by the Swarm observations in the northern hemisphere, but with various tilt angles. From the Swarm spacecrafts with zonal separations of about 150 km, we conclude that larger zonal scale sizes of irregularities exist during the early evening hours (around 1900 LT).
The reservoir sediments are important sinks for organic carbon (OC), the OC burial being dependent on two opposite processes, deposition and mineralization. Hence factors such as severe water level fluctuations are expected to influence the rate of OC accumulation as they may affect both deposition and mineralization. The Barasona Reservoir has been historically threatened by siltation, whilst the use of water for irrigation involves a drastic decrease of the water level. In this context, we have studied the physical and chemical characteristics (grain size, major and minor elemental compositions, organic and inorganic carbon, and nitrogen) of the recent sediments of the Barasona Reservoir and the relationships among them in order to: a) elucidate the main processes governing OC accumulation, b) evaluate the rate of OC mineralization and c) approach the effect of drought on the sediment characteristics in this system. Our results indicated that Barasona sediments were dominated by fine silts (>60%) and clays (>20%), the mean particle size decreasing from tail to dam. Desiccation increased particle sorting and size distribution became bimodal, but no effect on average size was observed. Attending to the composition, Barasona sediments were very homogeneous with low concentrations of nitrogen (TN) and phosphorus (<12 g kg(-1) dw and <0.6 g kg(-1) dw, respectively) and high concentration of OC (approximate to 36 kg(-1) dw). TN was negatively related to dry weight Sediment mixing due to drastic changes in water level may have favoured the observed homogeneity of Barasona sediments affecting carbon, major ions and grain size. The high amount of OC deposited in Barasona sediment suggested that the adsorption of OC onto fine particles was more important than in boreal lakes. The rate of oxygen consumption by wet sediment ranged from 2.26 to 3.15 mg O-2 m(-2) day(-1), values close to those compiled for Mediterranean running waters. (C) 2015 Elsevier B.V. All rights reserved.
Regulation alters the characteristics of riversty transforming parts of them into lakes, affecting their hydrology and also the physical, chemical, and biological characteristics and dynamics. Reservoirs have proven to be very effective retaining particulate materials, thereby avoiding the downstream transport of suspended sediment and the chemical substances associated with it (e.g. Carbon, C or Nitrogen, N). The study of fluvial transport of C and N is of great interest since river load represents a major link to the global C and N cycles. Moreover, reservoirs are the most important sinks for organic carbon among inland waters and have a potential significance as nitrogen sinks. In this respect, this paper investigates the effects of a Pyrenean reservoir on the runoff, suspended sediment, C and N derived from the highly active Esera and Isabena rivets. Key findings indicate that the reservoir causes a considerable impact on the Esera-Isabena river fluxes, reducing them dramatically as almost all the inputs are retained within the reservoir. Despite the very dry study year (2011-2012), it can be calculated that almost 300,000 t of suspended sediment were deposited into the Barasona Reservoir, from which more than 16,000 were C (i.e. 2200 t as organic C) and 222 t were N. These values may not be seen as remarkable in a wider global context but, assuming that around 30 hm(3) of sediment are currently stored in the reservoir, figures would increase up to ca. 2.6 x 10(6) t of C (i.e. 360,000 t of organic C) and 35,000 t of N. Nevertheless, these values are indicative and should be treated with caution as there is incomplete understanding of all the processes which affect C and N. Further investigation to establish a more complete picture of C and N yields and budgets by monitoring the different processes involved is essential. (C) 2015 Elsevier B.V. All rights reserved.
Mediterranean climate is characterized by highly irregular rainfall patterns with marked differences between wet and dry seasons which lead to highly variable hydrological fluvial regimes. As a result, and in order to ensure water availability and reduce its temporal variability, a high number of large dams were built during the 20th century (more than 3500 located in Mediterranean rivers). Dams modify the flow regime but also interrupt the continuity of sediment transfer along the river network, thereby changing its functioning as an ecosystem. Within this context, the present paper aims to assess the suspended sediment loads and dynamics of two climatically contrasting Mediterranean regulated rivers (i.e. the Esera and Siurana) during a 2-yr period. Key findings indicate that floods were responsible for 92% of the total suspended sediment load in the River Siurana, while this percentage falls to 70% for the Esera, indicating the importance of baseflows on sediment transport in this river. This fact is related to the high sediment availability, with the Esera acting as a non-supply-limited catchment due to the high productivity of the sources (i.e. badlands). In contrast, the Siurana can be considered a supply-limited system due to its low geomorphic activity and reduced sediment availability, with suspended sediment concentration remaining low even for high magnitude flood events. Reservoirs in both rivers reduce sediment load up to 90%, although total runoff is only reduced in the case of the River Esera. A remarkable fact is the change of the hydrological character of the River Lem downstream for the dam, shifting from a humid mountainous river regime to a quasi-invariable pattern, whereas the Siurana experiences the opposite effect, changing from a flashy Mediterranean river to a more constant flow regime below the dam. (C) 2015 Elsevier B.V. All rights reserved.
The uppermost Cretaceous (upper Campanian-Maastrichtian) marine deposits of the central south Pyrenees host a rich larger benthic foraminiferal fauna and several rudist-rich levels. These marine deposits are directly overlain by the continental facies of the Aren and Tremp Formations, which are famous for their fossil dinosaur remains. Larger benthic foraminiferal distribution documents an important faunal turnover in all the carbonate platform environments within the photic zone, from open marine to littoral areas. Biostratigraphy indicates that this turnover occurred close to the Campanian-Maastrichtian boundary. This is also confirmed by strontium isotope stratigraphy which indicates an earliest Maastrichtian age for the appearance of the larger benthic foraminiferal assemblage constituted by Lepidorbitoides socialis, Clypeorbis mammillata, Wannierina cataluniensis, Orbitoides gruenbachensis, Siderolites aff. calcitrapoides, Fascispira colomi, Omphalocyclus macroporus and Laffiteina mengaudi. In particular, a numerical age of 71 Ma is obtained for the Hippurites radiosus level, just a few meters below the first continental deposits of the Aren sensu stricto Formation. The youngest marine sediments of the central south Pyrenees are early Maastrichtian in age. This is also an important constraint for the age of the end-Cretaceous dinosaur fossil localities of the Tremp basin. (C) 2015 Elsevier Ltd. All rights reserved.
Sarmentofascis zamparelliae n. sp., a new demosponge from the lower Campanian of southern Italy
(2016)
A new coralline sponge, exhibiting typical "stromatoporoid" bodyplan, is described as Sarmentofascis zamparelliae n. sp. from the lower Campanian of the southern Apennines, Italy. It is differentiated from Sarmentofascis cretacea (Turnsek) (Hauterivian of Montenegro) and Sarmentofascis chabrieri Termier, Termier and Vachard (Santonian of France) above all by its slender arborescent skeleton, exhibiting longitudinally distributed astrorhizae-like canals. S. zamparelliae n. sp. is the youngest representative of the genus and is reported from a period exhibiting a distinct decline of "stromatoporoid" sponges. With its clinogonal microstructure and occurrence in inner platform stromatoporoid-foraminiferan floatstones it can be considered a Late Cretaceous environmental analog to the Late Jurassic Cladocoropsis. (C) 2015 Elsevier Ltd. All rights reserved.