Unterschiede
Hier werden die Unterschiede zwischen zwei Versionen angezeigt.
Beide Seiten der vorigen Revision Vorhergehende Überarbeitung Nächste Überarbeitung | Vorhergehende ÜberarbeitungLetzte ÜberarbeitungBeide Seiten der Revision | ||
thesis:mthesis:lateralflowsglobal [2017/12/06 16:36] – i.degraaf | thesis:mthesis:lateralflowsglobal [2019/02/28 10:09] – i.degraaf | ||
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- | ===== Should we include lateral groundwater flows in global-scale hydrological models? | + | ===== Global Scale Groundwater Flows (2 projects) ===== |
== Background == | == Background == | ||
+ | Should we include lateral groundwater flows in global-scale hydrological models? | ||
+ | |||
Groundwater is the world’s largest accessible source of freshwater and plays a vital role in satisfying basic need of human society. During dry periods, groundwater storage provides a natural buffer against water shortage, preserves evaporation in areas with shallow water tables, and sustains baseflows to rives and wetlands. Also, groundwater often flows across catchment boundaries at considerable rates, supporting water budgets of receiving catchments. Despite the importance of groundwater, | Groundwater is the world’s largest accessible source of freshwater and plays a vital role in satisfying basic need of human society. During dry periods, groundwater storage provides a natural buffer against water shortage, preserves evaporation in areas with shallow water tables, and sustains baseflows to rives and wetlands. Also, groundwater often flows across catchment boundaries at considerable rates, supporting water budgets of receiving catchments. Despite the importance of groundwater, | ||
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Kollet and Maxwell (2008), Capturing the influence of groundwater dynamics on land surface processes using an integrated, distributed watershed model, WRR. | Kollet and Maxwell (2008), Capturing the influence of groundwater dynamics on land surface processes using an integrated, distributed watershed model, WRR. | ||
- | {{tag> | + | {{tag> |