Land–atmosphere coupling (LAC) is a critical process in the climate system, and has great
effects on surface air temperature over the humid–dry transition zones. Using ERA5/ERA5 …

Soil moisture is an important parameter in land surface processes, which can control the
surface energy and water budgets and thus affect the air temperature. Studying the coupling …

Land–atmosphere coupling is a crucial factor influencing extreme weather and climate.
Based on the ERA5‐Land reanalysis data set and sensitivity experiments with the CESM1 …

Examining large-scale characteristics of the difference between ground surface temperature
(GST) and surface air temperature (SAT) and its long-term trend will help understand land …

Significant temporal and spatial variability in soil moisture (SM) is observed during the warm
season in China and its surrounding regions. Because of the existence of two different …

Land–atmosphere coupling is a key process of the climate system, and various coupling
mechanisms have been proposed before based on observational and numerical analyses …

Arid regions suffer seriously from frequent and severe heatwaves. As compared to other
regions, however, the synoptic-scale characteristics and mechanism of heatwave events in …

The surface-air temperature difference (Ts-Ta) is the main contributor to the sensible heat
flux, and also an important indicator for land degradation. However, as the main influencing …

The impact of soil moisture initialization on the 2016 Northeast Asian heat wave was
explored using the Land Information System (LIS) Weather Research and Forecasting …

Climate extremes, such as extreme hot temperatures and heat waves, can have dramatic
societal, economic, and ecological consequences. China has experienced remarkable …