The Noah-MP land surface model (LSM) relies on the Monin-Obukhov (M-O) Similarity Theory (MOST) to calculate land-atmosphere exchanges of water, energy, and momentum fluxes. However, MOST flux-profile relationships neglect canopy-induced turbulence in roughness sublayer (RSL) parameterize within-canopy an ad hoc manner. We implement a new physics scheme (M-O-RSL) into that explicitly parameteri...

Land surface schemes (LSSs) in Earth System Models simulate how vegetation regulates land-atmosphere fluxes of heat, water, carbon, and momentum. Despite advances the spatial resolution regional climate modeling, significant land cover changes occured at sub-grid scale still not properly treated. Here, we investigate response evapotranspiration, representing heat to deforestation Southeast Asia...

Land surface processes play a vital role in the exchange of momentum, energy, and mass between land atmosphere. However, current model simplifies canopy structure using approximately three to six parameters, which makes representation radiation energy distribution uncertain large extent. To improve simulation performance, more specific parameters were retrieved by UAV-LiDAR observation system u...

This study applies three widely used land models (SSiB, CLM, and Noah-MP) coupled in a regional climate model to quantitatively assess their skill preserving the imposed ± 5 °C anomalies on initial surface subsurface temperature (LST/SUBT) generating 2-m air (T2m) over Tibetan Plateau (TP) during May–August. The memory of LST/SUBT (surface/soil memory) is defined as first time when series diffe...