Modeling has become an indispensable tool for scientific research. However, models
generate great uncertainty when they are used to predict or forecast ecosystem responses to …

Most ecological and environmental issues faced by human society can only be solved at the
ecosystem, watershed, regional and even global scale. Thus, ecological research is …

Soil microbial respiration is an important source of uncertainty in projecting future climate
and carbon (C) cycle feedbacks. However, its feedbacks to climate warming and underlying …

Permafrost thaw could trigger the release of greenhouse gases through microbial
decomposition of the large quantities of carbon (C) stored within frozen soils. However …

Increases in carbon (C) inputs to soil can replenish soil organic C (SOC) through various
mechanisms. However, recent studies have suggested that the increased C input can also …

Increasingly, the human existence in urban environments is growing. In addition,
anthropogenic activity has altered the global carbon (C) cycle and triggered climate change …

Abstract Effects of permafrost degradation on carbon (C) and nitrogen (N) cycling on the
Qinghai‐Tibetan Plateau (QTP) have rarely been analyzed. This study used a revised …

Global nitrogen (N) deposition substantially enhances ecosystem carbon cycling but usually
results in minor carbon sequestration. The mechanisms underlying the minor stimulation of …

The sustainability of the vast Arctic permafrost carbon pool under climate change is of
paramount importance for global climate trajectories. Accurate climate change forecasts …

Climate warming is accelerating the changes in the global terrestrial ecosystems and
particularly those in the northern high latitudes (NHLs; poleward of 50∘ N) and rendering …