The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood
flux in the global carbon cycle. Climatic warming is hypothesized to increase rates of soil …

Global climate warming may induce a positive feedback through increasing soil carbon (C)
release to the atmosphere. Although warming can affect both C input to and output from soil …

Soil respiration (R s) represents the largest flux of CO2 from terrestrial ecosystems to the
atmosphere, but its spatial and temporal changes as well as the driving forces are not well …

Changing precipitation regimes could have profound influences on carbon (C) cycle in the
biosphere. However, how soil C release from terrestrial ecosystems responds to changing …

Warming-induced carbon loss through terrestrial ecosystem respiration (Re) is likely getting
stronger in high latitudes and cold regions because of the more rapid warming and higher …

Global warming intensifies the hydrological cycle, which results in changes in precipitation
regime (frequency and amount), and will likely have significant impacts on soil respiration (R …

Forage nutrient storages can determine livestock size and husbandry development. There is
insufficient research on the response of forage nutrient storages to grazing and related …

As a widespread direct effect of global warming, drought is currently wreaking havoc on
terrestrial ecosystems' structure and function, however, the synthesized analysis is lacked to …

Evaluating the responses of soil respiration and its components to global environmental
change is crucial for predicting future terrestrial carbon cycle. However, the effects of …

Responses of soil respiration (R s) to increasing nitrogen (N) deposition and warming will
have far-reaching influences on global carbon (C) cycling. However, the seasonal (growing …