Climate controls fire regimes through its influence on the amount and types of fuel present and their dryness. CO2 concentration constrains primary production by limiting photosynthetic activity in plants. However, although fuel accumulation depends on biomass production, and hence on CO2 concentration, the quantitative relationship between atmospheric CO2 concentration and biomass burning is not well understood. Here a fire-enabled dynamic global vegetation model (the Land surface Processes and eXchanges model, LPX) is used to attribute glacial–interglacial changes in biomass burning to an increase in CO2, which would be expected to increase primary production and therefore fuel loads even in the absence of climate change, vs. climate chan...
Temperature exerts strong controls on the incidence and severity of fire. All else equal, warming i...
[1] Wildfire is a common occurrence in ecosystems of northern high latitudes, and changes in the fir...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
Climate controls fire regimes through its influence on the amount and types of fuel present and thei...
Climate controls fire regimes through its influence on the amount and types of fuel present and thei...
This project uses the Land Processes and eXchanges (LPX) model to analyse fire-vegetation-climate in...
Dynamic global vegetation models (DGVMs) can disentangle causes and effects in the control of vegeta...
[1] Climate at the Last Glacial Maximum (LGM) together with low atmospheric CO2 concentration forced...
•In current models, the ecophysiological effects of CO2 create both woody thickening and terrestrial...
Temperature exerts strong controls on the incidence and severity of fire. All else equal, warming is...
). To date, the global-scale climate response of controlling emission of these constituents together...
International audienceVegetation reconstructions from pollen data for the Last Glacial Maximum (LGM)...
International audienceCarbon dioxide emissions from wild and anthropogenic fires return the carbon a...
Fire is an important natural disturbance factor, which significantly impacts vegetation dynamics. Fi...
The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative...
Temperature exerts strong controls on the incidence and severity of fire. All else equal, warming i...
[1] Wildfire is a common occurrence in ecosystems of northern high latitudes, and changes in the fir...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
Climate controls fire regimes through its influence on the amount and types of fuel present and thei...
Climate controls fire regimes through its influence on the amount and types of fuel present and thei...
This project uses the Land Processes and eXchanges (LPX) model to analyse fire-vegetation-climate in...
Dynamic global vegetation models (DGVMs) can disentangle causes and effects in the control of vegeta...
[1] Climate at the Last Glacial Maximum (LGM) together with low atmospheric CO2 concentration forced...
•In current models, the ecophysiological effects of CO2 create both woody thickening and terrestrial...
Temperature exerts strong controls on the incidence and severity of fire. All else equal, warming is...
). To date, the global-scale climate response of controlling emission of these constituents together...
International audienceVegetation reconstructions from pollen data for the Last Glacial Maximum (LGM)...
International audienceCarbon dioxide emissions from wild and anthropogenic fires return the carbon a...
Fire is an important natural disturbance factor, which significantly impacts vegetation dynamics. Fi...
The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative...
Temperature exerts strong controls on the incidence and severity of fire. All else equal, warming i...
[1] Wildfire is a common occurrence in ecosystems of northern high latitudes, and changes in the fir...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...