The Central Asia region is covered by vast desert ecosystems, where the characteristic of energy and water fluxes is different from other humid ecosystems. The application of land surface models (LSMs) in arid and semiarid ecosystems was largely limited. This paper presents a detailed evaluation of Common Land Model (CoLM) at two eddy covariance (EC) sites in alkaline desert ecosystems over Central Asia. Simulations of the net radiation (Rnet), latent heat flux (Qle), sensible heat flux (Qh), and soil temperature showed that refined estimate of roughness length (Z0m) significantly improved the performance of CoLM in simulating turbulent heat fluxes. Qle was increased but Qh was decreased, which were in better agreement with the observations...
Shortfalls in regular evapotranspiration (ET) monitoring and evaluation pose a huge challenge to agr...
Current land surface models still have difficulties with producing reliable surface heat fluxes and ...
A simple model of surface and sub -surface soil temperature was developed at the watershed scale ( -...
The ability of roots to take up water depends on both root distribution and root water uptake effici...
Improving and validating land surface models based on integrated observations in deserts is one of t...
Relatively small fluctuations in the surface energy balance and evapotranspiration in semiarid and a...
The oases in the mountain-basin systems of Central Asia are extremely fragile. Investigating oasis e...
A land-surface physical process model was coupled with a mesoscale atmospheric model. This coupled m...
The Land surface scheme is crucial for the performance of regional climate models in dynamic downsca...
Accurate estimation of latent heat flux (LE) is critical in characterizing semiarid ecosystems. Many...
The accurate estimation of global evapotranspiration (ET) is essential to understanding the water cy...
While land-atmosphere transfer models have been pursued for over 30 years, Soil-Vegctalion-Almosphcr...
Quantifying the surface energy fluxes of grazed and ungrazed steppes is essential to understand the ...
The Common Land Model (CLM) is one of the most widely used land surface models (LSMs) due to the pra...
By extending Modified Soil-Plant-Atmosphere Scheme (MSPAS) to include an effective parameterization ...
Shortfalls in regular evapotranspiration (ET) monitoring and evaluation pose a huge challenge to agr...
Current land surface models still have difficulties with producing reliable surface heat fluxes and ...
A simple model of surface and sub -surface soil temperature was developed at the watershed scale ( -...
The ability of roots to take up water depends on both root distribution and root water uptake effici...
Improving and validating land surface models based on integrated observations in deserts is one of t...
Relatively small fluctuations in the surface energy balance and evapotranspiration in semiarid and a...
The oases in the mountain-basin systems of Central Asia are extremely fragile. Investigating oasis e...
A land-surface physical process model was coupled with a mesoscale atmospheric model. This coupled m...
The Land surface scheme is crucial for the performance of regional climate models in dynamic downsca...
Accurate estimation of latent heat flux (LE) is critical in characterizing semiarid ecosystems. Many...
The accurate estimation of global evapotranspiration (ET) is essential to understanding the water cy...
While land-atmosphere transfer models have been pursued for over 30 years, Soil-Vegctalion-Almosphcr...
Quantifying the surface energy fluxes of grazed and ungrazed steppes is essential to understand the ...
The Common Land Model (CLM) is one of the most widely used land surface models (LSMs) due to the pra...
By extending Modified Soil-Plant-Atmosphere Scheme (MSPAS) to include an effective parameterization ...
Shortfalls in regular evapotranspiration (ET) monitoring and evaluation pose a huge challenge to agr...
Current land surface models still have difficulties with producing reliable surface heat fluxes and ...
A simple model of surface and sub -surface soil temperature was developed at the watershed scale ( -...