TY - BOOK A1 - Bahouth, Chadi T1 - Der Konflikt um Wasser in Israel und Palästina BT - Konfliktstoff trotz Friedensquells – die vergebene Chance einer nachhaltigen und gerechten Lösung N2 - Wasser ist rar im Nahen Osten. Die knappe Ressource wird immer häufiger zum Gegenstand politischer Konflikte in der ohnehin instabilen Region. Der Konflikt zwischen Israel und Palästina gilt als eines der gravierendsten Beispiele für diese Entwicklung: Wasser als umkämpftes Menschenrecht, Wasser als strategisches Mittel der Besetzungspolitik und Wasser als Gegenstand langwieriger Verhandlungen. Der Wasserkonflikt ist so alt wie der Nahostkonflikt selbst. Sogar mit Beginn des Oslo-Prozesses 1993 hat es weder einen grundlegenden Wandel im Wasserkonflikt, noch in der Aussicht auf Veränderung der Wasserknappheit gegeben. Immerhin können die Palästinenser in der momentanen Situation ihre eigene Wasserversorgung dort selbst verwalten, wo es ihnen laut der Übereinkünfte erlaubt ist. Jedoch ist diese Freiheit eine sehr begrenzte und eine endgültige Klärung dieses Streitpunktes wurde, zusammen mit Jerusalem, den Flüchtlingen, den Siedlungen und der Staatsbildung auf die Endstatusverhandlungen verschoben. Chadi Bahouth, Absolvent des Otto-Suhr-Instituts der Freien Universität Berlin, untersucht in seiner Doktorarbeit die Gründe für die ungelöste Wasserfrage. Er analysiert die historische und rechtliche Chronologie des Konfliktes, bietet Lösungsvorschläge für die Wasserkrise an und erklärt, warum die Region dennoch für Generationen nicht zur Ruhe kommen wird. N2 - Water is rare at the Middle East and becomes more and more a matter of political conflicts in the already instable region. The conflict between Israel and Palestine is a serious noticeable example of this development: water as a hard-fought human right, water as a strategic mean of the politics of occupation and water as a matter of protracted negotiations. The battles for water are as old as the Middle East conflict itself. Even with the beginning of the Oslo-Process in 1993 there has not been a fundamental change containing the water conflict. After all, the Palestinians in the actual situation can administrate their own water supply, where they are allowed to concern the accords. But this freedom is strictly confined and a clarification of the controversial subject, together with Jerusalem, the refugees, the settlements and the building of the state were adjusted to the negotiations of the permanent status. Chadi Bahouth, alumnus of the Otto-Suhr-Institute (Free University Berlin), inspects in his doctoral thesis the reasons for the unsolved water politics. He analyses the historical and judicial chronology of the conflict, offers proposals for solution and explains, why the region will not be steadied for generations, nevertheless. T3 - Horizonte 21 : Umwelt · Energie · Sicherheit - 2 KW - Nahostkonflikt KW - Israel KW - Palästina KW - Wasser KW - Friedensprozess KW - Middle-East Conflict KW - Israel KW - Palestine KW - water KW - peace process Y1 - 2010 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-40747 SN - 978-3-86956-035-9 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - JOUR A1 - Baritello, Omar A1 - Khajooei, Mina A1 - Engel, Tilman A1 - Kopinski, Stephan A1 - Quarmby, Andrew James A1 - Müller, Steffen A1 - Mayer, Frank T1 - Neuromuscular shoulder activity during exercises with different combinations of stable and unstable weight mass JF - BMC sports science, medicine and rehabilitation N2 - Background Recent shoulder injury prevention programs have utilized resistance exercises combined with different forms of instability, with the goal of eliciting functional adaptations and thereby reducing the risk of injury. However, it is still unknown how an unstable weight mass (UWM) affects the muscular activity of the shoulder stabilizers. Aim of the study was to assess neuromuscular activity of dynamic shoulder stabilizers under four conditions of stable and UWM during three shoulder exercises. It was hypothesized that a combined condition of weight with UWM would elicit greater activation due to the increased stabilization demand. Methods Sixteen participants (7 m/9 f) were included in this cross-sectional study and prepared with an EMG-setup for the: Mm. upper/lower trapezius (U.TA/L.TA), lateral deltoid (DE), latissimus dorsi (LD), serratus anterior (SA) and pectoralis major (PE). A maximal voluntary isometric contraction test (MVIC; 5 s.) was performed on an isokinetic dynamometer. Next, internal/external rotation (In/Ex), abduction/adduction (Ab/Ad) and diagonal flexion/extension (F/E) exercises (5 reps.) were performed with four custom-made-pipes representing different exercise conditions. First, the empty-pipe (P; 0.5 kg) and then, randomly ordered, water-filled-pipe (PW; 1 kg), weight-pipe (PG; 4.5 kg) and weight + water-filled-pipe (PWG; 4.5 kg), while EMG was recorded. Raw root-mean-square values (RMS) were normalized to MVIC (%MVIC). Differences between conditions for RMS%MVIC, scapular stabilizer (SR: U.TA/L.TA; U.TA/SA) and contraction (CR: concentric/eccentric) ratios were analyzed (paired t-test; p <= 0.05; Bonferroni adjusted alpha = 0.008). Results PWG showed significantly greater muscle activity for all exercises and all muscles except for PE compared to P and PW. Condition PG elicited muscular activity comparable to PWG (p > 0.008) with significantly lower activation of L.TA and SA in the In/Ex rotation. The SR ratio was significantly higher in PWG compared to P and PW. No significant differences were found for the CR ratio in all exercises and for all muscles. Conclusion Higher weight generated greater muscle activation whereas an UWM raised the neuromuscular activity, increasing the stabilization demands. Especially in the In/Ex rotation, an UWM increased the RMS%MVIC and SR ratio. This might improve training effects in shoulder prevention and rehabilitation programs. KW - EMG KW - instability KW - overhead athlete KW - unstable resistance training KW - water KW - pipe KW - rotator cuff Y1 - 2020 U6 - https://doi.org/10.1186/s13102-020-00168-x SN - 2052-1847 VL - 12 IS - 1 PB - BioMed Central CY - London ER - TY - GEN A1 - Block, Inga A1 - Günter, Christina A1 - Rodrigues, Alysson Duarte A1 - Paasch, Silvia A1 - Hesemann, Peter A1 - Taubert, Andreas T1 - Carbon Adsorbents from Spent Coffee for Removal of Methylene Blue and Methyl Orange from Water T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Activated carbons (ACs) were prepared from dried spent coffee (SCD), a biological waste product, to produce adsorbents for methylene blue (MB) and methyl orange (MO) from aqueous solution. Pre-pyrolysis activation of SCD was achieved via treatment of the SCD with aqueous sodium hydroxide solutions at 90 °C. Pyrolysis of the pretreated SCD at 500 °C for 1 h produced powders with typical characteristics of AC suitable and effective for dye adsorption. As an alternative to the rather harsh base treatment, calcium carbonate powder, a very common and abundant resource, was also studied as an activator. Mixtures of SCD and CaCO3 (1:1 w/w) yielded effective ACs for MO and MB removal upon pyrolysis needing only small amounts of AC to clear the solutions. A selectivity of the adsorption process toward anionic (MO) or cationic (MB) dyes was not observed. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1155 KW - water KW - spent coffee KW - dye adsorption KW - methylene blue KW - methyl orange KW - calcium carbonate KW - activated carbon KW - water treatment KW - dye removal Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-521653 SN - 1866-8372 IS - 14 ER - TY - JOUR A1 - Block, Inga A1 - Günter, Christina A1 - Rodrigues, Alysson Duarte A1 - Paasch, Silvia A1 - Hesemann, Peter A1 - Taubert, Andreas T1 - Carbon Adsorbents from Spent Coffee for Removal of Methylene Blue and Methyl Orange from Water JF - Materials N2 - Activated carbons (ACs) were prepared from dried spent coffee (SCD), a biological waste product, to produce adsorbents for methylene blue (MB) and methyl orange (MO) from aqueous solution. Pre-pyrolysis activation of SCD was achieved via treatment of the SCD with aqueous sodium hydroxide solutions at 90 °C. Pyrolysis of the pretreated SCD at 500 °C for 1 h produced powders with typical characteristics of AC suitable and effective for dye adsorption. As an alternative to the rather harsh base treatment, calcium carbonate powder, a very common and abundant resource, was also studied as an activator. Mixtures of SCD and CaCO3 (1:1 w/w) yielded effective ACs for MO and MB removal upon pyrolysis needing only small amounts of AC to clear the solutions. A selectivity of the adsorption process toward anionic (MO) or cationic (MB) dyes was not observed. KW - water KW - spent coffee KW - dye adsorption KW - methylene blue KW - methyl orange KW - calcium carbonate KW - activated carbon KW - water treatment KW - dye removal Y1 - 2021 U6 - https://doi.org/10.3390/ma14143996 SN - 1996-1944 VL - 14 IS - 14 PB - MDPI CY - Basel ER - TY - GEN A1 - Duy, Nguyen Le A1 - Heidbüchel, Ingo A1 - Meyer, Hanno A1 - Merz, Bruno A1 - Apel, Heiko T1 - What controls the stable isotope composition of precipitation in the Mekong Delta? BT - a model-based statistical approach T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - This study analyzes the influence of local and regional climatic factors on the stable isotopic composition of rainfall in the Vietnamese Mekong Delta (VMD) as part of the Asian monsoon region. It is based on 1.5 years of weekly rainfall samples. In the first step, the isotopic composition of the samples is analyzed by local meteoric water lines (LMWLs) and single-factor linear correlations. Additionally, the contribution of several regional and local factors is quantified by multiple linear regression (MLR) of all possible factor combinations and by relative importance analysis. This approach is novel for the interpretation of isotopic records and enables an objective quantification of the explained variance in isotopic records for individual factors. In this study, the local factors are extracted from local climate records, while the regional factors are derived from atmospheric backward trajectories of water particles. The regional factors, i.e., precipitation, temperature, relative humidity and the length of backward trajectories, are combined with equivalent local climatic parameters to explain the response variables delta O-18, delta H-2, and d-excess of precipitation at the station of measurement. The results indicate that (i) MLR can better explain the isotopic variation in precipitation (R-2 = 0.8) compared to single-factor linear regression (R-2 = 0.3); (ii) the isotopic variation in precipitation is controlled dominantly by regional moisture regimes (similar to 70 %) compared to local climatic conditions (similar to 30 %); (iii) the most important climatic parameter during the rainy season is the precipitation amount along the trajectories of air mass movement; (iv) the influence of local precipitation amount and temperature is not sig-nificant during the rainy season, unlike the regional precipitation amount effect; (v) secondary fractionation processes (e.g., sub-cloud evaporation) can be identified through the d-excess and take place mainly in the dry season, either locally for delta O-18 and delta H-2, or along the air mass trajectories for d-excess. The analysis shows that regional and local factors vary in importance over the seasons and that the source regions and transport pathways, and particularly the climatic conditions along the pathways, have a large influence on the isotopic composition of rainfall. Although the general results have been reported qualitatively in previous studies (proving the validity of the approach), the proposed method provides quantitative estimates of the controlling factors, both for the whole data set and for distinct seasons. Therefore, it is argued that the approach constitutes an advancement in the statistical analysis of isotopic records in rainfall that can supplement or precede more complex studies utilizing atmospheric models. Due to its relative simplicity, the method can be easily transferred to other regions, or extended with other factors. The results illustrate that the interpretation of the isotopic composition of precipitation as a recorder of local climatic conditions, as for example performed for paleorecords of water isotopes, may not be adequate in the southern part of the Indochinese Peninsula, and likely neither in other regions affected by monsoon processes. However, the presented approach could open a pathway towards better and seasonally differentiated reconstruction of paleoclimates based on isotopic records. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 927 KW - Asian summer monsoon KW - interannuel variability KW - climate controls KW - deuterium excess KW - oxygen isotopes KW - paleoclimate KW - water KW - system KW - trajectories KW - circulation Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-445743 SN - 1866-8372 IS - 927 SP - 1239 EP - 1262 ER - TY - GEN A1 - Fondell, Mattis A1 - Eckert, Sebastian A1 - Jay, Raphael Martin A1 - Weniger, Christian A1 - Quevedo, Wilson A1 - Niskanen, Johannes A1 - Kennedy, Brian A1 - Sorgenfrei, Nomi A1 - Schick, Daniel A1 - Giangrisostomi, Erika A1 - Ovsyannikov, Ruslan A1 - Adamczyk, Katrin A1 - Huse, Nils A1 - Wernet, Philippe A1 - Mitzner, Rolf A1 - Föhlisch, Alexander T1 - Time-resolved soft X-ray absorption spectroscopy in transmission mode on liquids at MHz repetition rates T2 - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe N2 - We present a setup combining a liquid flatjet sample delivery and a MHz laser system for time-resolved soft X-ray absorption measurements of liquid samples at the high brilliance undulator beamline UE52-SGM at Bessy II yielding unprecedented statistics in this spectral range. We demonstrate that the efficient detection of transient absorption changes in transmission mode enables the identification of photoexcited species in dilute samples. With iron(II)-trisbipyridine in aqueous solution as a benchmark system, we present absorption measurements at various edges in the soft X-ray regime. In combination with the wavelength tunability of the laser system, the set-up opens up opportunities to study the photochemistry of many systems at low concentrations, relevant to materials sciences, chemistry, and biology. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 780 KW - l-edge xas KW - electronic-structure KW - molecular-structure KW - spin-state KW - dynamics KW - complexes KW - probe KW - water KW - iron(II) KW - spectra Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-437529 SN - 1866-8372 IS - 780 ER - TY - JOUR A1 - Guzman, Diego A. A1 - Samprogna Mohor, Guilherme A1 - Mendiondo, Eduardo Mario T1 - Multi-year index-based insurance for adapting Water Utility Companies to hydrological drought BT - case study of a water supply system of the Sao Paulo metropolitan region, Brazil JF - Water N2 - The sustainability of water utility companies is threatened by non-stationary drivers, such as climate and anthropogenic changes. To cope with potential economic losses, instruments such as insurance are useful for planning scenarios and mitigating impacts, but data limitations and risk uncertainties affect premium estimation and, consequently, business sustainability. This research estimated the possible economic impacts of business interruption to the Sao Paulo Water Utility Company derived from hydrological drought and how this could be mitigated with an insurance scheme. Multi-year insurance (MYI) was proposed through a set of "change" drivers: the climate driver, through forcing the water evaluation and planning system (WEAP) hydrological tool; the anthropogenic driver, through water demand projections; and the economic driver, associated with recent water price policies adopted by the utility company during water scarcity periods. In our study case, the evaluated indices showed that MYI contracts that cover only longer droughts, regardless of the magnitude, offer better financial performance than contracts that cover all events (in terms of drought duration). Moreover, through MYI contracts, we demonstrate solvency for the insurance fund in the long term and an annual average actuarially fair premium close to the total expected revenue reduction. KW - multi-year insurance KW - climate change KW - hydrological drought KW - water KW - security and economy Y1 - 2020 U6 - https://doi.org/10.3390/w12112954 SN - 2073-4441 VL - 12 IS - 11 PB - MDPI CY - Basel ER - TY - THES A1 - Hunke, Philip Paul T1 - The Brazilian Cerrado: ecohydrological assessment of water and soil degradation in heavily modified meso-scale catchments T1 - Der brasilianische Cerrado: ökohydrologische Analyse von Boden- und Wasserdegradierung in intensiv landwirtschaftlich genutzten mesoskaligen Einzugsgebieten N2 - The Brazilian Cerrado is recognised as one of the most threatened biomes in the world, as the region has experienced a striking change from natural vegetation to intense cash crop production. The impacts of rapid agricultural expansion on soil and water resources are still poorly understood in the region. Therefore, the overall aim of the thesis is to improve our understanding of the ecohydrological processes causing water and soil degradation in the Brazilian Cerrado. I first present a metaanalysis to provide quantitative evidence and identifying the main impacts of soil and water alterations resulting from land use change. Second, field studies were conducted to (i) examine the effects of land use change on soils of natural cerrado transformed to common croplands and pasture and (ii) indicate how agricultural production affects water quality across a meso-scale catchment. Third, the ecohydrological process-based model SWAT was tested with simple scenario analyses to gain insight into the impacts of land use and climate change on the water cycling in the upper São Lourenço catchment which experienced decreasing discharges in the last 40 years. Soil and water quality parameters from different land uses were extracted from 89 soil and 18 water studies in different regions across the Cerrado. Significant effects on pH, bulk density and available P and K for croplands and less-pronounced effects on pastures were evident. Soil total N did not differ between land uses because most of the cropland sites were N-fixing soybean cultivations, which are not artificially fertilized with N. By contrast, water quality studies showed N enrichment in agricultural catchments, indicating fertilizer impacts and potential susceptibility to eutrophication. Regardless of the land use, P is widely absent because of the high-fixing capacities of deeply weathered soils and the filtering capacity of riparian vegetation. Pesticides, however, were consistently detected throughout the entire aquatic system. In several case studies, extremely high-peak concentrations exceeded Brazilian and EU water quality limits, which pose serious health risks. My field study revealed that land conversion caused a significant reduction in infiltration rates near the soil surface of pasture (–96 %) and croplands (–90 % to –93 %). Soil aggregate stability was significantly reduced in croplands than in cerrado and pasture. Soybean crops had extremely high extractable P (80 mg kg–1), whereas pasture N levels declined. A snapshot water sampling showed strong seasonality in water quality parameters. Higher temperature, oxi-reduction potential (ORP), NO2–, and very low oxygen concentrations (<5 mg•l–1) and saturation (<60 %) were recorded during the rainy season. By contrast, remarkably high PO43– concentrations (up to 0.8 mg•l–1) were measured during the dry season. Water quality parameters were affected by agricultural activities at all sampled sub-catchments across the catchment, regardless of stream characteristic. Direct NO3– leaching appeared to play a minor role; however, water quality is affected by topsoil fertiliser inputs with impact on small low order streams and larger rivers. Land conversion leaving cropland soils more susceptible to surface erosion by increased overland flow events. In a third study, the field data were used to parameterise SWAT. The model was tested with different input data and calibrated in SWAT-CUP using the SUFI-2 algorithm. The model was judged reliable to simulate the water balance in the Cerrado. A complete cerrado, pasture and cropland cover was used to analyse the impact of land use on water cycling as well as climate change projections (2039–2058) according to the projections of the RCP 8.5 scenario. The actual evapotranspiration (ET) for the cropland scenario was higher compared to the cerrado cover (+100 mm a–1). Land use change scenarios confirmed that deforestation caused higher annual ET rates explaining partly the trend of decreased streamflow. Taking all climate change scenarios into account, the most likely effect is a prolongation of the dry season (by about one month), with higher peak flows in the rainy season. Consequently, potential threats for crop production with lower soil moisture and increased erosion and sediment transport during the rainy season are likely and should be considered in adaption plans. From the three studies of the thesis I conclude that land use intensification is likely to seriously limit the Cerrado’s future regarding both agricultural productivity and ecosystem stability. Because only limited data are available for the vast biome, we recommend further field studies to understand the interaction between terrestrial and aquatic systems. This thesis may serve as a valuable database for integrated modelling to investigate the impact of land use and climate change on soil and water resources and to test and develop mitigation measures for the Cerrado in the future. N2 - Ökohydrologische Interaktionen in Folge von exzessiver Bodenerosion auf landwirtschaftlich stark modifizierten Flächen können speziell in tropischen Gebieten einen großen Einfluss auf die Fruchtbarkeit und zukünftige Nutzbarkeit der Böden haben, wie dies im Cerrado geschieht. Der brasilianische Cerrado ist eine neotropische Savanne und stellt mit 2 Mio. km² das zweitgrößte Biom Südamerikas dar. Das Biom wird global unter den bedeutendsten aber auch meist gefährdetsten 25 Biodiversitätshotspots gelistet. Ein extremer Landnutzungswandel führt dazu, dass der Cerrado zu den weltweit bedeutendsten landwirtschaftlichen Gebieten zählt und mittlerweile > 50 % des Bioms abgeholzt sind. Durch staatliche Subventionsprogramme, Aufkalkung und Düngung der Böden werden mehrere Ernten (v.a. Soja, Mais, Zuckerrohr und Baumwolle) pro Jahr bei hohem Ertrag realisiert. Aufgrund weniger Untersuchungen ist bisher unklar, wie sich die Landnutzungsintensivierung mit dem Einsatz großer Mengen an Agrochemikalien auf die Boden- und Wasserressourcen auswirkt. Um die Zielsetzung zu erreichen, wurden in einer umfassenden Metaanalyse Boden- und Wasserqualitätsparameter von mehr als 100 Einzelstudien analysiert, mehrere Feldkampagnen zur Erhebung bodenphysikochemischer und Wasserqualitätsparameter für unterschiedliche Landnutzungen durchgeführt und Modellierungen mit SWAT zur Abschätzung des Landnutzungs- und Klimawandels vorgenommen. Die Literaturanalyse konnte zeigen, dass Erosion, Veränderungen des Nährstoffkreislaufs, Nährstoffanreicherungen und sehr hohe Pestizidkonzentrationen in den Gewässern des gesamten Cerrado auftreten, mit stärkster Ausprägung für Ackerflächen. Trotz hoher Düngemengen wird festgestellt, dass P nur in sehr geringen Konzentrationen in den Gewässern nachgewiesen wird, welches auf die P-Fixierung der Böden und die Filterleistung der Uferrandstreifen zurückzuführen ist. In einer Feldstudie bestätigen sich die Ergebnisse, dass der Landnutzungswandel zu deutlichen Änderungen der boden-physikochemischen Parameter führt, wie z.B. einer signifikanten Abnahme der hydraulischen Leitfähigkeit (> –90 %) und der Bodenaggregatstabilität. Außerdem werden erhöhte pH-Werte und Überdüngung anzeigende P und K-gehalte im Oberboden (9-fach natürlicher Hintergrund) mit der stärksten Ausprägung unter Soja gemessen. Die Niederschlagsintensitäten überschreiten die Infiltrationskapazität der landwirtschaftlich genutzten Böden, wodurch es zu erhöhtem Oberflächenabfluss, Bodenerosionsereignissen mit Gullyformierungen kommt und der Eintrag von Agrochemikalien in die zuvor pristinen Gewässer begünstigt wird. Verglichen mit natürlichen Gewässern konnten im gesamten Einzugsgebiet niedrigere O2-Werte (< 5 mg l–1) sowie erhöhte NO3– (0.5 mg l–1), NO2– (0.1 mg l–1) und in der Trockenzeit auf direkte Düngung zurückzuführende sehr hohe PO43– (0.8 mg l–1) Konzentrationen festgestellt werden. Da in den Bodenprofilen keine Tiefenakkumulation von NPK nachgewiesen wurde ist davon auszugehen, dass Dünger durch Oberflächenabflussprozesse in das Flusssystem gelangen. Auch wenn die Nährstoffkonzentrationen nach europäischen Maßstäben gering sind, ist anzunehmen, dass in einem nährstofflimitierten System wie dem Cerrado die um ein vielfach erhöhte Konzentration der natürlichen Hintergrundwerte den Metabolismus der Gewässer negativ beeinflusst. In einer dritten Studie wird mit SWAT untersucht wie sich der Landnutzungs- und Klimawandel auf die Wasserbilanz auswirkt. In Testläufen zeigt sich, dass sowohl die verwendeten Niederschlagseingangsdaten als auch die Vegetationsparameter des natürlichen Cerrados von hoher Relevanz sind. Die Simulation verschiedener Landnutzungsszenarien belegt, dass die im Gebiet beobachteten abnehmenden Abflüsse auf die Zunahme landwirtschaftlicher Produktion und einer damit einhergehenden Zunahme der Evapotranspiration zurückzuführen sind. Die Simulation extremer Klimaszenarien (RCP 8.5 2039-2058) verdeutlicht, dass sich die Trockenzeit verlängert, welches Auswirkungen auf die Aussaattermine haben könnte. Gleichzeitig nehmen die Spitzenabflüsse in der Regenzeit zu, welches ohne entsprechende Gegenmaßnahmen zu erhöhter Erosion und gesteigertem Nähr- und Schadstofftransport in die Gewässer führt. Kombiniert mit einer weiteren Landnutzungsintensivierung wird für die zukünftige Entwicklung des Cerrado geschlussfolgert, dass die Veränderungen des Wasser- und Nährstoffhaushalt durch die Landwirtschaft und die damit einhergehenden Degradierungserscheinungen die Produktivität und Ökosystemstabilität nicht dauerhaft gewährleisten werden können. Die vorliegende Dissertation liefert einen zentralen Beitrag zur ökohydrologischen Bewertung des Status quo und der zukünftigen Entwicklung des brasilianischen Cerrados. Sie kann einen Ausgangspunkt für weitere Forschungen und Modellierungen darstellen, um die in dieser Arbeit benannten offenen Fragen hinsichtlich der ökohydrologischen Interaktionen zu klären. KW - Cerrado KW - ecohydrology KW - water KW - soil KW - deforestation KW - Cerrado KW - Ökohydrologie KW - Landnutzung KW - Boden KW - Wasser Y1 - 2015 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-85110 ER - TY - GEN A1 - Lara, Mark J. A1 - Nitze, Ingmar A1 - Große, Guido A1 - McGuire, David T1 - Tundra landform and vegetation productivity trend maps for the Arctic Coastal Plain of northern Alaska T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Arctic tundra landscapes are composed of a complex mosaic of patterned ground features, varying in soil moisture, vegetation composition, and surface hydrology over small spatial scales (10-100 m). The importance of microtopography and associated geomorphic landforms in influencing ecosystem structure and function is well founded, however, spatial data products describing local to regional scale distribution of patterned ground or polygonal tundra geomorphology are largely unavailable. Thus, our understanding of local impacts on regional scale processes (e.g., carbon dynamics) may be limited. We produced two key spatiotemporal datasets spanning the Arctic Coastal Plain of northern Alaska (similar to 60,000 km(2)) to evaluate climate-geomorphological controls on arctic tundra productivity change, using (1) a novel 30m classification of polygonal tundra geomorphology and (2) decadal-trends in surface greenness using the Landsat archive (1999-2014). These datasets can be easily integrated and adapted in an array of local to regional applications such as (1) upscaling plot-level measurements (e.g., carbon/energy fluxes), (2) mapping of soils, vegetation, or permafrost, and/or (3) initializing ecosystem biogeochemistry, hydrology, and/or habitat modeling. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1035 KW - spatial-distribution KW - lake basins KW - microtopography KW - water KW - ice KW - accumulation KW - degradation KW - permafrost KW - dynamics KW - barrow Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-459875 SN - 1866-8372 IS - 1035 ER - TY - JOUR A1 - Lehr, Christian A1 - Lischeid, Gunnar T1 - Efficient screening of groundwater head monitoring data for anthropogenic effects and measurement errors JF - Hydrology and Earth System Sciences N2 - 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. KW - streamflow variability KW - principal components KW - united states KW - time-seriesa KW - water KW - network KW - nonstationarity KW - fluctuations KW - rotation Y1 - 2020 U6 - https://doi.org/10.5194/hess-24-501-2020 SN - 1027-5606 SN - 1607-7938 VL - 24 IS - 2 SP - 501 EP - 513 PB - Copernicus CY - Göttingen ER -