![]() ![]() In this study, the multiphysics version of the Noah land‐surface model (Noah‐MP) was used to identify the processes, which are most crucial for a simultaneous simulation of water and heat fluxes between land surface and the lower atmosphere. ![]() However, land‐surface schemes used in large‐scale models continue to show deficiencies in consistently simulating fluxes of water and energy from the subsurface through vegetation layers to the atmosphere. Interactions between the soil, the vegetation, and the atmospheric boundary layer require close attention when predicting water fluxes in the hydrogeosystem, agricultural systems, weather, and climate. ![]() Gayler, Sebastian Wöhling, Thomas Grzeschik, Matthias Ingwersen, Joachim Wizemann, Hans‐Dieter Warrach‐Sagi, Kirsten Högy, Petra Attinger, Sabine Streck, Thilo Wulfmeyer, Volker Incorporating dynamic root growth enhances the performance of Noah‐MP at two contrasting winter wheat field sites Incorporating dynamic root growth enhances the performance of Noah‐MP at two contrasting winter. ![]()
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