FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2398820199> ?p ?o ?g. }

• W2398820199 endingPage "2602" @default.
• W2398820199 startingPage "2590" @default.
• W2398820199 abstract "Abstract The Pantanal wetland is one of the least explored regions of South America. It is characterized by an outstanding flora and fauna adapted to a seasonal flood pulse controlled by a dry and a wet season within each year. The resulting inundation covers in average an area of approximately 150 000 km 2 and is seen as the most important driver for ecological integrity. Evaporation from the large floodplain is supposed to influence the climate of the whole continent. The regional groundwater is connected to the surface water and plays an important role for the characteristic flooding regime by regulating the wetland's water table. The water balance assessment of the wetland and the internal water exchange between surface and groundwater is therefore of high relevance for the conservation of the Pantanal biodiversity. Despite of its importance, water balance studies including groundwater–surface water interactions based on field data are rarely undertaken. This is mainly due to the remoteness and difficulty in accessing this area, which results in lack of data. In our study, we developed a new tracer‐based model to simulate the spatio–temporal surface and subsurface fluxes for a range of water bodies. The model was able to simulate these fluxes considering a dynamic simulation of inflow and outflow using a newly collected 2‐year dataset of water levels, stable water isotopes and chloride collected from several water bodies in the northern Pantanal region. Quantitative differences between water bodies according to their location in the floodplain were determined by the flooding regime and connectivity as well as site‐specific characteristics, such as hydraulic conductivity and water depth. Our model simulated water balance fluxes with a Nash–Sutcliffe efficiency of 0.61, whereas it simulated stable water isotopic compositions better than chloride. We present the first study based on field data for the Pantanal, which is able to quantify water balances fluxes. Because their representation in global climate and land cover products is insufficient, our simulation results are valuable for validating large‐scale models. Copyright © 2016 John Wiley & Sons, Ltd." @default.
• W2398820199 created "2016-06-24" @default.
• W2398820199 creator A5046697227 @default.
• W2398820199 creator A5067442586 @default.
• W2398820199 creator A5074109419 @default.
• W2398820199 date "2016-06-12" @default.
• W2398820199 modified "2023-10-05" @default.
• W2398820199 title "A tracer-based simulation approach to quantify seasonal dynamics of surface-groundwater interactions in the Pantanal wetland" @default.
• W2398820199 cites W133058041 @default.
• W2398820199 cites W1537170892 @default.
• W2398820199 cites W1600484632 @default.
• W2398820199 cites W1631149859 @default.
• W2398820199 cites W169873142 @default.
• W2398820199 cites W179065688 @default.
• W2398820199 cites W1909649765 @default.
• W2398820199 cites W1989293071 @default.
• W2398820199 cites W1993892615 @default.
• W2398820199 cites W1993901853 @default.
• W2398820199 cites W1997132492 @default.
• W2398820199 cites W2039952687 @default.
• W2398820199 cites W2057173141 @default.
• W2398820199 cites W2065290873 @default.
• W2398820199 cites W2067692525 @default.
• W2398820199 cites W2102406667 @default.
• W2398820199 cites W2118989103 @default.
• W2398820199 cites W2120561153 @default.
• W2398820199 cites W2127170577 @default.
• W2398820199 cites W2162719469 @default.
• W2398820199 cites W2171706312 @default.
• W2398820199 cites W2173160686 @default.
• W2398820199 cites W2411181024 @default.
• W2398820199 cites W2480650616 @default.
• W2398820199 cites W2505264646 @default.
• W2398820199 cites W2949691538 @default.
• W2398820199 cites W4241090273 @default.
• W2398820199 cites W566720969 @default.
• W2398820199 cites W97725961 @default.
• W2398820199 doi "https://doi.org/10.1002/hyp.10904" @default.
• W2398820199 hasPublicationYear "2016" @default.
• W2398820199 type Work @default.
• W2398820199 sameAs 2398820199 @default.
• W2398820199 citedByCount "8" @default.
• W2398820199 countsByYear W23988201992017 @default.
• W2398820199 countsByYear W23988201992019 @default.
• W2398820199 countsByYear W23988201992021 @default.
• W2398820199 countsByYear W23988201992022 @default.
• W2398820199 crossrefType "journal-article" @default.
• W2398820199 hasAuthorship W2398820199A5046697227 @default.
• W2398820199 hasAuthorship W2398820199A5067442586 @default.
• W2398820199 hasAuthorship W2398820199A5074109419 @default.
• W2398820199 hasConcept C127313418 @default.
• W2398820199 hasConcept C1284942 @default.
• W2398820199 hasConcept C155681218 @default.
• W2398820199 hasConcept C15744967 @default.
• W2398820199 hasConcept C166957645 @default.
• W2398820199 hasConcept C186594467 @default.
• W2398820199 hasConcept C187320778 @default.
• W2398820199 hasConcept C18903297 @default.
• W2398820199 hasConcept C205649164 @default.
• W2398820199 hasConcept C39432304 @default.
• W2398820199 hasConcept C39769621 @default.
• W2398820199 hasConcept C542102704 @default.
• W2398820199 hasConcept C58640448 @default.
• W2398820199 hasConcept C66465714 @default.
• W2398820199 hasConcept C67715294 @default.
• W2398820199 hasConcept C74256435 @default.
• W2398820199 hasConcept C75622301 @default.
• W2398820199 hasConcept C76177295 @default.
• W2398820199 hasConcept C76886044 @default.
• W2398820199 hasConcept C8625798 @default.
• W2398820199 hasConcept C86803240 @default.
• W2398820199 hasConcept C87717796 @default.
• W2398820199 hasConcept C9777977 @default.
• W2398820199 hasConceptScore W2398820199C127313418 @default.
• W2398820199 hasConceptScore W2398820199C1284942 @default.
• W2398820199 hasConceptScore W2398820199C155681218 @default.
• W2398820199 hasConceptScore W2398820199C15744967 @default.
• W2398820199 hasConceptScore W2398820199C166957645 @default.
• W2398820199 hasConceptScore W2398820199C186594467 @default.
• W2398820199 hasConceptScore W2398820199C187320778 @default.
• W2398820199 hasConceptScore W2398820199C18903297 @default.
• W2398820199 hasConceptScore W2398820199C205649164 @default.
• W2398820199 hasConceptScore W2398820199C39432304 @default.
• W2398820199 hasConceptScore W2398820199C39769621 @default.
• W2398820199 hasConceptScore W2398820199C542102704 @default.
• W2398820199 hasConceptScore W2398820199C58640448 @default.
• W2398820199 hasConceptScore W2398820199C66465714 @default.
• W2398820199 hasConceptScore W2398820199C67715294 @default.
• W2398820199 hasConceptScore W2398820199C74256435 @default.
• W2398820199 hasConceptScore W2398820199C75622301 @default.
• W2398820199 hasConceptScore W2398820199C76177295 @default.
• W2398820199 hasConceptScore W2398820199C76886044 @default.
• W2398820199 hasConceptScore W2398820199C8625798 @default.
• W2398820199 hasConceptScore W2398820199C86803240 @default.
• W2398820199 hasConceptScore W2398820199C87717796 @default.
• W2398820199 hasConceptScore W2398820199C9777977 @default.
• W2398820199 hasIssue "15" @default.
• W2398820199 hasLocation W23988201991 @default.

• next