Permafrost thaw can cause an intensification of climate change through the release of
carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well …

Groundwater-surface water (GW-SW) interaction, as a key component in the cold region
hydrologic cycle, is extremely sensitive to seasonal and climate change. Specifically, the …

Permafrost thaw can accelerate climate warming by releasing carbon from previously frozen
soil in the form of greenhouse gases. Rainfall extremes have been proposed to increase …

Permafrost thaw leads to an increase in groundwater circulation and potential mobilization
of organic carbon sequestered in deep Arctic sediments (eg 3–25 m below surface). Upon …

为从整体上认识多年冻土流域水循环过程基本规律及其对下垫面条件变化响应,
以长江源区风火山小流域为例, 基于2016—2019 年的水文气象要素的野外观测与计算 …

Northern high-latitudes are projected to get warmer and wetter, which will affect rates of
permafrost thaw and mechanisms by which thaw occurs. To better understand the impact of …

Together with warming air temperatures, Arctic ecosystems are expected to experience
increases in heavy rainfall events. Recent studies report accelerated degradation of …

In Arctic landscapes, the active layer forms a near‐surface aquifer on top of the permafrost
where water and nutrients are available for plants or subject to downslope transport. Warmer …

Abstract Study region The Qinghai-Tibetan Plateau (QTP) is the highest plateau in the world
and has been recognized as the “Asia water tower”. Frozen soils in China are mostly …

Increasing greenhouse gas levels drive extensive changes in Arctic and cold‐dominated
environments, leading to a warmer, more humid, and variable climate. Associated …