Permafrost regions at high latitudes and altitudes store about half of the Earth's soil organic
carbon (SOC). These areas are also some of the most intensely affected by anthropogenic …

It is important to investigate the responses of greenhouse gases to climate change
(temperature, precipitation) and anthropogenic factors in plateau wetland. Based on the …

Rapid climate change and intensified anthropogenic disturbances have dropped
groundwater level and altered hydrology conditions, provoked the drought-induced …

The imbalance of terrestrial carbon (C) inputs versus losses to extreme precipitation can
have consequences for ecosystem carbon balances. However, the current understanding of …

One of the major uncertainties for projecting permafrost carbon (C)‐climate feedback is a
poor representation of the non‐growing season carbon dioxide (CO2) emissions under a …

Alpine grasslands play important functions in mitigating climate change and regulating water
resources. However, the spatiotemporal variability of their carbon and water budgets …

Hydrological changes under climate warming drive the biogeomorphic succession of
wetlands and may trigger substantial carbon loss from the carbon-rich ecosystems. Although …

Freezing and thawing profoundly affect soil carbon cycling. Under the influence of climate
change, rising temperatures and glacier shrinkage in arid regions have increased the spring …

Soil respiration (Rs) is the largest flux of carbon dioxide (CO2) next to photosynthesis in
terrestrial ecosystems. With the absorption of atmospheric methane (CH4), upland soils …

Wetlands sequestrate carbon at the highest rate than any other ecosystems on Earth.
However, the spatial and temporal dynamics of GHGs emissions from the wetland …