Enhanced frequency and intensity of freeze-thaw cycle (FTC) owing to global climate
change may influence soil carbon (C) and phosphorus (P) cycling in terrestrial ecosystems …

Changes in characteristics of snowfall and spring freeze–thaw-cycle (FTC) events under the
warming climate make it critical to understand biophysical controls on soil CO2 efflux (RS) in …

As an important factor regulating soil carbon cycle, freeze-thaw cycle significantly affects
winter soil respiration in temperate regions. However, few in situ studies have been carried …

The COVID-19 pandemic has changed all areas of human activity as it forced the authorities
around the world to enact unprecedented restrictions such as “lockdowns”. The low …

Forests can play a key role in the mitigation of climate change, although there have been
limited regional scale assessments that account for variations in soil type and tree species …

Climate change might alter annual snowfall patterns and modify the duration and magnitude
of snow cover in temperate regions with resultant impacts on soil microclimate and soil CO2 …

Measurements of the land‐atmosphere exchange of the greenhouse gases methane (CH4)
and carbon dioxide (CO2) in high Arctic tundra ecosystems are particularly difficult in the …

At high latitudes, the climate has warmed at twice the rate of the global average with most
changes observed in autumn, winter and spring. Increasing winter temperatures and wide …

As crucial terrestrial ecosystems, temperate forests play an important role in global soil
carbon dioxide flux and this process can be sensitive to atmospheric nitrogen deposition. It …

The release of water during snowmelt orchestrates a variety of important belowground
biogeochemical processes in seasonally snow‐covered ecosystems, including the …