Permafrost is warming at a rate of two times faster than the rest of the Earth's surface. However, there is still a lack of a quantitative basis for predicting the functional stability of permafrost ecosystems in carbon (C) and nutrient cycling. We compiled the data of 708 observations from 89 air-warming experiments in the Northern Hemisphere and characterized the general effects of temperature increase on permafrost C exchange and balance, biomass production, microbial biomass, soil nutrients, and vegetation N dynamics via a meta-analysis. Also, an investigation was made on how responses may change with habitat-specific (e.g., plant functional groups and soil moisture status) conditions and warming variables (e.g., warming phases, levels,...
International audiencePermafrost soils contain enormous amounts of organic carbon, which could act a...
Soil carbon in permafrost ecosystems has the potential to become a major positive feedback to climat...
Responses of ecosystem carbon (C) fluxes to human disturbance and climatic warming will affect terre...
Permafrost is warming at a rate of two times faster than the rest of the Earth's surface. However, t...
Large uncertainties exist in carbon (C)-climate feedback in permafrost regions, partly due to an ins...
In the last few decades, temperatures in the Arctic have increased twice as much as the rest of the ...
The global climate is predicted to become significantly warmer over the next century. This will affe...
Rapid Arctic warming is expected to increase global greenhouse gas concentrations as permafrost thaw...
Almost half of the global terrestrial soil carbon (C) is stored in the northern circumpolar permafro...
© 2016 Macmillan Publishers Limited, part of Springer Nature. Increasing temperatures in northern hi...
Climate warming can result in both abiotic (e.g., permafrost thaw) and biotic (e.g., microbial funct...
Plants may slow global warming through enhanced growth, because increased levels of photosynthesis s...
© The Author(s), 2016. This is the author's version of the work and is distributed under the terms o...
Permafrost soils contain more than 1300 Pg of carbon (C), twice the amount of C in the atmosphere. T...
Climate warming affects permafrost soil carbon pools in two opposing ways: enhanced vegetation growt...
International audiencePermafrost soils contain enormous amounts of organic carbon, which could act a...
Soil carbon in permafrost ecosystems has the potential to become a major positive feedback to climat...
Responses of ecosystem carbon (C) fluxes to human disturbance and climatic warming will affect terre...
Permafrost is warming at a rate of two times faster than the rest of the Earth's surface. However, t...
Large uncertainties exist in carbon (C)-climate feedback in permafrost regions, partly due to an ins...
In the last few decades, temperatures in the Arctic have increased twice as much as the rest of the ...
The global climate is predicted to become significantly warmer over the next century. This will affe...
Rapid Arctic warming is expected to increase global greenhouse gas concentrations as permafrost thaw...
Almost half of the global terrestrial soil carbon (C) is stored in the northern circumpolar permafro...
© 2016 Macmillan Publishers Limited, part of Springer Nature. Increasing temperatures in northern hi...
Climate warming can result in both abiotic (e.g., permafrost thaw) and biotic (e.g., microbial funct...
Plants may slow global warming through enhanced growth, because increased levels of photosynthesis s...
© The Author(s), 2016. This is the author's version of the work and is distributed under the terms o...
Permafrost soils contain more than 1300 Pg of carbon (C), twice the amount of C in the atmosphere. T...
Climate warming affects permafrost soil carbon pools in two opposing ways: enhanced vegetation growt...
International audiencePermafrost soils contain enormous amounts of organic carbon, which could act a...
Soil carbon in permafrost ecosystems has the potential to become a major positive feedback to climat...
Responses of ecosystem carbon (C) fluxes to human disturbance and climatic warming will affect terre...