Abstract The Tibetan Plateau (TP) exerts strong thermal forcing on the atmosphere over
Asian monsoon region and supplies water resources to adjacent river basins. Recently, the …

This review surveys the basic theories, observational methods, satellite algorithms, and land
surface models for terrestrial evapotranspiration, E (or λE, ie, latent heat flux), including a …

Abstract The Tibetan Plateau (TP) plays a critical role in influencing regional and global
climate, via both thermal and dynamical mechanisms. Meanwhile, as the largest high …

In the Arctic, climate warming enhances vegetation activity by extending the length of the
growing season and intensifying maximum rates of productivity. In turn, increased vegetation …

The parameterization of thermal roughness length z0h plays a key role in land surface
modeling. Previous studies have found that the daytime land surface temperature (LST) on …

Abstract The Tibetan Plateau (TP) surfaces have been experiencing an overall rapid
warming and wetting while wind speed and solar radiation have been declining in the last …

Soil moisture is a key state variable in many hydrological processes. The Global Land Data
Assimilation System (GLDAS) can produce global and continuous soil moisture data sets …

We review recent climate changes over the Tibetan Plateau (TP) and associated responses
of cryospheric, biospheric, and hydrological variables. We focused on surface air …

A multi‐scale soil moisture and temperature monitoring network, consisting of 55 soil
moisture and temperature measurement stations, has been established in central Tibetan …

Long-term and large-scale reanalysis products of soil temperature and soil moisture are very
important for understanding the hydrothermal regime in permafrost regions. However, it is …