For short-lived climate forcers (SLCFs), the impact of emissions depends on where and when the emissions take place. Comprehensive new calculations of various emission metrics for SLCFs are presented based on radiative forcing (RF) values calculated in four different (chemical-transport or coupled chemistry–climate) models. We distinguish between emissions during summer (May–October) and winter (November–April) for emissions in Europe and East Asia, as well as from the global shipping sector and global emissions. The species included in this study are aerosols and aerosol precursors (BC, OC, SO2, NH3), as well as ozone precursors (NOx, CO, VOCs), which also influence aerosols to a lesser degree. Emission metrics for global climate responses...
We compare future changes in global mean temperature in response to different future scenarios which...
Bien que plusieurs études suggèrent que l’exposition à la chaleur, au froid ou aux particules en sus...
Substantial changes in anthropogenic aerosols and precursor gas emissions have occurred over recent ...
We calculate the absolute regional temperature change potential (ARTP) of various short-lived clima...
For short-lived climate forcers (SLCFs), the impact of emissions depends on where and when the emis...
Predictions of temperature and precipitation responses to changes in the anthropogenic emissions of ...
While cumulative carbon dioxide (CO2) emissions dominate anthropogenic warming over centuries, tempe...
Multi-model ensembles are frequently used to assess understanding of the response of ozone and metha...
International audienceThis paper presents a summary of the work done within the European Union's Sev...
Parties to the United Nations Framework Convention on Climate Change (UNFCCC) have requested guidanc...
Recent advances in understanding have made it possible to relate global precipitation changes direct...
Most emission metrics have previously been inconsistently estimated by including the climate-carbon ...
While carbon dioxide is the main cause for global warming, modeling short-lived climate forcers (SLC...
Climate risks increase with mean global temperature, so knowledge about the amount of future global ...
Short-lived anthropogenic climate forcers (SLCFs), such as sulfate aerosols, affect both climate and...
We compare future changes in global mean temperature in response to different future scenarios which...
Bien que plusieurs études suggèrent que l’exposition à la chaleur, au froid ou aux particules en sus...
Substantial changes in anthropogenic aerosols and precursor gas emissions have occurred over recent ...
We calculate the absolute regional temperature change potential (ARTP) of various short-lived clima...
For short-lived climate forcers (SLCFs), the impact of emissions depends on where and when the emis...
Predictions of temperature and precipitation responses to changes in the anthropogenic emissions of ...
While cumulative carbon dioxide (CO2) emissions dominate anthropogenic warming over centuries, tempe...
Multi-model ensembles are frequently used to assess understanding of the response of ozone and metha...
International audienceThis paper presents a summary of the work done within the European Union's Sev...
Parties to the United Nations Framework Convention on Climate Change (UNFCCC) have requested guidanc...
Recent advances in understanding have made it possible to relate global precipitation changes direct...
Most emission metrics have previously been inconsistently estimated by including the climate-carbon ...
While carbon dioxide is the main cause for global warming, modeling short-lived climate forcers (SLC...
Climate risks increase with mean global temperature, so knowledge about the amount of future global ...
Short-lived anthropogenic climate forcers (SLCFs), such as sulfate aerosols, affect both climate and...
We compare future changes in global mean temperature in response to different future scenarios which...
Bien que plusieurs études suggèrent que l’exposition à la chaleur, au froid ou aux particules en sus...
Substantial changes in anthropogenic aerosols and precursor gas emissions have occurred over recent ...