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Hydrological model uncertainty due to spatial evapotranspiration estimation methods

Evapotranspiration (ET) continues to be a difficult process to estimate in seasonal and long-term water balances in catchment models. Approaches to estimate ET typically use vegetation parameters (e.g., leaf area index [LAI], interception capacity) o...

DA - Hydrologie a limnologie

  • 2016
  • Jx
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