Spatial and temporal predictions of soil moisture patterns and evaporative losses using TOPMODEL and the GASFLUX model for an Alaskan catchment

• Published in: Hydrology and Earth System Sciences
• Main Authors: Quinn, P. F., Ostendorf, B., Beven, K., Tenhunen, J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 1998
• Subjects: article; Verlagsveröffentlichung; Tundra; Alaska
• Online Access: https://doi.org/10.5194/hess-2-51-1998; https://noa.gwlb.de/receive/cop_mods_00037346; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037300/hess-2-51-1998.pdf; https://hess.copernicus.org/articles/2/51/1998/hess-2-51-1998.pdf

By using topographic indices as derived from a Digital Terrain Models (DTM), it is possible to represent the heterogeneity within a landscape. This heterogeneity can reflect both long term evolutionary patterns seen in a landscape and the short term forcing of flow dynamics during storm events. By spatial analysis, the linkage between the geomorphological- hydrological-plant physiological phenomena can be examined. In this study, a direct link will be established between the topographically-driven hydrological phenomena and the eco-physiological response. The topographic distribution function of TOPMODEL is used to control the spatial and temporal flux of the channel flow and water table. The plant physiological model GAS-FLUX is used to give a spatially and temporally dissaggregated species-sensitive estimate of evapotranspiration flux. Evapotranspiration is sensitive to the vegetation phonology, to tundra community physiology and to the temperature regime. A simple linking of TOPMODEL and the GAS-FLUX model is applied to a summer snow-free period to the Imnavait catchment, Alaska (2.2 km2). A species-sensitive evapotranspiration model proved to give the highest quality results when validated against flow observations. Predicted dynamics of variable source area and the component hydrological processes are illustrated.