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Catchment hydrologic response with a fully distributed triangulated irregular network model
Author(s) -
Ivanov Valeriy Y.,
Vivoni Enrique R.,
Bras Rafael L.,
Entekhabi Dara
Publication year - 2004
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2004wr003218
Subject(s) - vadose zone , hydrology (agriculture) , watershed , surface runoff , distributed element model , environmental science , interception , hydrological modelling , terrain , drainage basin , catchment hydrology , evapotranspiration , routing (electronic design automation) , discretization , computer science , geology , soil science , soil water , geography , mathematics , ecology , cartography , geotechnical engineering , climatology , computer network , mathematical analysis , physics , quantum mechanics , machine learning , biology
This study explores various aspects of catchment hydrology based on a mechanistic modeling of distributed watershed processes. A new physics‐based, distributed‐parameter hydrological model that uses an irregular spatial discretization is introduced. The model accounts, on a continuous basis, for the processes of rainfall interception, evapotranspiration, moisture dynamics in the unsaturated and saturated zones, and runoff routing. Simulations of several mid‐ to large‐sized watersheds (∼10 3 km 2 ) highlight various dynamic relationships between the vadose zone–groundwater processes and their dependence on the land surface characteristics. It is argued that the model inferences can be used for interpretation of distributed relationships in a catchment. By exploiting a multiple‐resolution representation, the hydrologic features of the watershed terrain are captured with only 5–10% of the original grid nodes. This computational efficiency suggests the feasibility of the operational use of fully distributed, physics‐based models for large watersheds.