Cryospheric changes and their impacts have received increasing concern, extending the
research to include the interactions between earth spheres and the impacts of and social …

Soil hydrological processes are extremely complex in high-altitude regions and are
recognized to have positive effects on soil quality, nutrient cycling, herbage yield, and runoff …

The effective restoration of degraded areas, resulting in the sequestration of significant
amounts of soil organic carbon (SOC) and labile soil organic carbon fractions (LOCF), is …

As a buffer layer for the energy and water exchange between atmosphere and permafrost,
the active layer is sensitive to climate warming. Changes in the thermal state in active layer …

Vegetation restoration is an effective strategy for sequestering soil organic carbon (SOC)
and restoring degraded ecosystems. However, the effects of different restoration strategies …

Many investigations of the preservation of soil organic carbon (SOC) in permafrost regions
have examined roles of geomorphology, pedogenesis, vegetation cover, and permafrost …

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 …

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 …

Soil texture data are the basic input parameters for many Earth System Models. As the
largest middle–low altitude permafrost regions on the planet, the land surface processes on …

The response of dissolved organic carbon (DOC) flux to permafrost degradation is one of the
major sources of uncertainty in predicting the permafrost carbon feedback. We investigated …