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 …

Plant‐mediated CH 4 flux is an important pathway for land–atmosphere CH 4 emissions, but
the magnitude, timing, and environmental controls, spanning scales of space and time …

The role of inland water in CO 2 exchange with the atmosphere was evaluated on the basis
of calculated partial pressure of CO 2 (pCO 2) from sampling of 207 lakes and 84 reservoirs …

As surface temperatures are expected to rise in the future, ice‐rich permafrost may thaw,
altering soil topography and hydrology and creating a mosaic of wet and dry soil surfaces in …

Climate change is warming tundra ecosystems in the Arctic, resulting in the decomposition
of previously-frozen soil organic matter (SOM) and release of carbon (C) to the atmosphere; …

Arctic wetlands are currently net sources of atmospheric CH 4. Due to their complex
biogeochemical controls and high spatial and temporal variability, current net CH 4 …

Permafrost landscapes in northern high latitudes with their massive organic carbon stocks
are an important, poorly known, component of the global carbon cycle. However, in light of …

In order to advance our understanding of the driving factors controlling carbon dynamics and
evolution of water quality in river-reservoir systems for the generation of hydropower, we …

Northeast China contains a large concentration of wetlands, primarily in two prominent
types, freshwater marshes on the lowlands plains to the northeast and mountain permafrost …

Hydrologic conditions are a key factor in Arctic ecosystems, with strong influences on
ecosystem structure and related effects on biogeophysical and biogeochemical processes …