Soil freeze–thaw processes are remarkable features of the land surface across the Tibetan Plateau (TP). Soil moisture and temperature fluctuate during the freeze–thaw cycle, affecting the soil water and energy exchange between the land and atmosphere. This study investigates variations in the soil temperature, humidity, and freeze–thaw state and their responses to air temperature and precipitation on the TP from 1981 to 2016. Regional simulations of the TP using Community Land Model version 4.5 demonstrate that the climate of the TP has become warmer and wetter over the past 37 years, with increases in both regional average temperature and precipitation. Using empirical orthogonal function analysis and the Mann–Kendall trend test of air tem...
The alpine ecosystem is very sensitive to environmental change due to global and local disturbances....
Since the 1990s, the Qinghai-Tibetan Plateau (QTP) has experienced a strikingly warming and wetter c...
The near-surface soil freeze/thaw status is an important indicator of climate change. Using data fro...
Abstract. Frozen soil processes are of great importance in controlling surface water and energy bala...
Climate warming has induced significant changes in permafrost and seasonally frozen ground (SFG) in ...
Soil moisture (SM), as a crucial variable in the soil–vegetation–atmosphere continuum, plays an impo...
Frozen soil properties and thermohydraulic processes are still not fully understood due to lack of i...
Soil freeze-thaw is typically not fully considered in quantifying the hydrology of seasonally frozen...
[1] In this paper we summarize recent research in geocryological studies carried out on the Qinghai-...
Abstract Soil water and heat transfer is especially complicated during the freezing and thawing proc...
Phenology is critical to ecosystem carbon quantification, and yet has not been well modeled consider...
Abstract Hydrothermal processes and the regimes of frozen soil formed in alpine regions with glacier...
The climatic conditions and soil characteristics of the Loess Plateau in China make it have a unique...
Understanding the driving forces for alpine vegetation variations at different permafrost degrading ...
The Tibetan alpine grasslands, sharing many features with arctic tundra ecosystems, have a unique no...
The alpine ecosystem is very sensitive to environmental change due to global and local disturbances....
Since the 1990s, the Qinghai-Tibetan Plateau (QTP) has experienced a strikingly warming and wetter c...
The near-surface soil freeze/thaw status is an important indicator of climate change. Using data fro...
Abstract. Frozen soil processes are of great importance in controlling surface water and energy bala...
Climate warming has induced significant changes in permafrost and seasonally frozen ground (SFG) in ...
Soil moisture (SM), as a crucial variable in the soil–vegetation–atmosphere continuum, plays an impo...
Frozen soil properties and thermohydraulic processes are still not fully understood due to lack of i...
Soil freeze-thaw is typically not fully considered in quantifying the hydrology of seasonally frozen...
[1] In this paper we summarize recent research in geocryological studies carried out on the Qinghai-...
Abstract Soil water and heat transfer is especially complicated during the freezing and thawing proc...
Phenology is critical to ecosystem carbon quantification, and yet has not been well modeled consider...
Abstract Hydrothermal processes and the regimes of frozen soil formed in alpine regions with glacier...
The climatic conditions and soil characteristics of the Loess Plateau in China make it have a unique...
Understanding the driving forces for alpine vegetation variations at different permafrost degrading ...
The Tibetan alpine grasslands, sharing many features with arctic tundra ecosystems, have a unique no...
The alpine ecosystem is very sensitive to environmental change due to global and local disturbances....
Since the 1990s, the Qinghai-Tibetan Plateau (QTP) has experienced a strikingly warming and wetter c...
The near-surface soil freeze/thaw status is an important indicator of climate change. Using data fro...