Abstract The Tibetan Plateau (TP) impacts local and remote atmospheric circulations,
wherein it mechanically and thermally affects air masses or airflows. Moreover, the TP …

Warming amplification over the Arctic Pole (AP hereafter) and Third Pole (Tibetan Plateau,
TP hereafter) can trigger a series of climate responses and have global consequences …

Abstract The Third Pole (TP) is experiencing rapid warming and is currently in its warmest
period in the past 2,000 years. This paper reviews the latest development in multidisciplinary …

Global warming has already had a significant impact on social ecosystems. The Tibetan
Plateau (TP), which is characterized by a cryosphere, is also recognized to have a profound …

Frost heave hazard is the uneven uplift of the ground surface due to the freezing of water
and the expansion of ice bodies in soil, especially in seasonally frozen soil. First, this study …

The changes in near-surface soil freeze-thaw cycles (FTCs) are crucial to understanding the
related hydrological and biological processes in terrestrial ecosystems under a changing …

Abstract The Yellow River source region is located in the transition region between
permafrost and seasonally frozen ground on the northeastern Qinghai-Tibet Plateau. The …

The source region of the Yellow River (SRYR) is greatly important for water resources
throughout the entire Yellow River Basin. Streamflow in the SRYR has experienced great …

Soil erosion measurements are important for land management and ecological restoration.
However, the current results of these measurements are varied and located in specific areas …

The freeze–thaw changes of seasonally frozen ground (SFG) are an important indicator of
climate change. Based on observed daily freeze depth of SFG from meteorological stations …