Forest soil CO2 efflux (FCO2) is a crucial process in global carbon cycling; however, how FCO2 responds to disturbance regimes in different forest biomes is poorly understood. We quantified the effects of disturbance regimes on FCO2 across boreal, temperate, tropical, and Mediterranean forests based on 1240 observations from 380 studies. Globally, climatic perturbations such as elevated CO2 concentration, warming, and increased precipitation increase FCO2 by 13 to 25%. FCO2 is increased by forest conversion to grassland and elevated carbon input by forest management practices but reduced by decreased carbon input, fire, and acid rain. Disturbance also changes soil temperature and water content, which in turn affect the direction and magnitu...
Forest ecosystems are often disturbed by agents such as harvesting, fire, wind, insects and diseases...
none8The response of ecosystems to environmental factors, such as temperature and rainfall, is cruci...
Determining soil carbon (C) responses to rising temperature is critical for projections of the feedb...
Soil CO2 efflux (FCO2) is a major component of the terrestrial carbon (C) cycle but challenges in ex...
Stem CO2 efflux (ES) plays an important role in the carbon balance of forest ecosystems. However, it...
The concentration of carbon dioxide (COx) in the atmosphere represents the balance between COx uptak...
Rises in anthropogenic CO2 emissions are now widely acknowledged to be responsible for changes in th...
The atmospheric carbon dioxide (CO2) concentrations have increased approximately 50% since the begin...
Alpine ecosystems are harsh environments where low temperatures are generally a limiting factor. Pre...
Alpine ecosystems are harsh environments where low temperatures are generally a limiting factor. Pre...
International audienceStem CO2 efflux (Es) is a significant component of total ecosystem respiration...
Soils of Northern Hemisphere forests contain a large part of the global terrestrial carbon (C) pool....
Carbon (C) fluxes are mainly controlled by small labile pools, and the C storage is determined by so...
Windthrow-driven changes in carbon (C) allocation and soil microclimate can affect soil carbon dioxi...
Forest ecosystems function as a significant carbon sink for atmospheric carbon dioxide. However, our...
Forest ecosystems are often disturbed by agents such as harvesting, fire, wind, insects and diseases...
none8The response of ecosystems to environmental factors, such as temperature and rainfall, is cruci...
Determining soil carbon (C) responses to rising temperature is critical for projections of the feedb...
Soil CO2 efflux (FCO2) is a major component of the terrestrial carbon (C) cycle but challenges in ex...
Stem CO2 efflux (ES) plays an important role in the carbon balance of forest ecosystems. However, it...
The concentration of carbon dioxide (COx) in the atmosphere represents the balance between COx uptak...
Rises in anthropogenic CO2 emissions are now widely acknowledged to be responsible for changes in th...
The atmospheric carbon dioxide (CO2) concentrations have increased approximately 50% since the begin...
Alpine ecosystems are harsh environments where low temperatures are generally a limiting factor. Pre...
Alpine ecosystems are harsh environments where low temperatures are generally a limiting factor. Pre...
International audienceStem CO2 efflux (Es) is a significant component of total ecosystem respiration...
Soils of Northern Hemisphere forests contain a large part of the global terrestrial carbon (C) pool....
Carbon (C) fluxes are mainly controlled by small labile pools, and the C storage is determined by so...
Windthrow-driven changes in carbon (C) allocation and soil microclimate can affect soil carbon dioxi...
Forest ecosystems function as a significant carbon sink for atmospheric carbon dioxide. However, our...
Forest ecosystems are often disturbed by agents such as harvesting, fire, wind, insects and diseases...
none8The response of ecosystems to environmental factors, such as temperature and rainfall, is cruci...
Determining soil carbon (C) responses to rising temperature is critical for projections of the feedb...