The current Northern Circumpolar Soil Carbon Database did not include organic carbon
storage in permafrost regions on the Qinghai–Xizang (Tibetan) Plateau (QXP). In this study …

In this study, we monitored a thaw slump in the permafrost region of the Qinghai–Tibet
Plateau in China, including its thaw settlement and solifluction creep characteristics, and …

There are several publications related to the soil organic carbon (SOC) on the Qinghai-
Tibetan Plateau (QTP). However, most of these reports were from different parts of the …

Important unknowns remain about how abrupt permafrost collapse (thermokarst) affects
carbon balance and greenhouse gas flux, limiting our ability to predict the magnitude and …

Antibiotic resistance genes (ARGs) and mobile genetic elements (MGEs) can be identified
with metagenomic analyses comparing relatively pristine and human-impacted …

While permafrost in the circum‐Artic has great influence on soil organic carbon (SOC) and
total nitrogen (TN) stocks, this might not be the case in low‐latitude arid permafrost regions …

Permafrost thaw subsidence, a key indicator of permafrost degradation, remains poorly
quantified or understood. It is particularly challenging to detect and measure surface …

The active layer plays a key role in geomorphic, hydrologic, and biogeochemical processes
in permafrost regions. We conducted a systematic investigation of active layer thickness …

Climate warming causes permafrost degradation that not only leads to the release of
greenhouse gases to the atmosphere, but also to soil moisture increases due to ground ice …

Permafrost collapse, known as thermokarst, can alter soil properties and carbon emissions.
However, little is known regarding the effects of permafrost collapse in upland landscapes …