Predictions of solar activity in the future are difficult to make due to the chaotic state of solar dynamo and the high nonlinearity of physical processes on the Sun. Therefore, the Climate Intercomparison Project Phase 6 (CMIP6) used a statistical approach and recommended two different solar forcing scenarios for the simulations. The reference scenario was developed as the standard forcing, whereas the alternative forcing has lower solar activity (EXT CMIP6). In this study, we use both forcings in a set of experiments to explore the importance of the alternative CMIP6 solar forcing for future climate and ozone layer variability. In general, the difference in solar forcing scenarios is small, and thus most changes at the surface and at high...
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with res...
The impact of changes in incoming solar irradiance on stratospheric ozone abundances should be inclu...
The 11 year solar‐cycle component of climate variability is assessed in historical simulations of mo...
International audienceThis paper describes the recommended solar forcing dataset for CMIP6 and highl...
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with res...
We estimate the consequences of a potential strong decrease of the solar activity using the model si...
The role of stratospheric ozone changes in determining the climate response to solar forcing is inve...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
We investigate the effects of a recently proposed 21st century Dalton minimum like decline of solar ...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
During the 20th century, solar activity increased in magnitude to a so-called grand maximum. It is p...
We apply two reconstructed spectral solar forcing scenarios, one SIM (Spectral Irradiance Monitor) b...
The 11-year solar cycle forcing is recognised as a potentially important atmospheric forcing; howeve...
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with res...
The impact of changes in incoming solar irradiance on stratospheric ozone abundances should be inclu...
The 11 year solar‐cycle component of climate variability is assessed in historical simulations of mo...
International audienceThis paper describes the recommended solar forcing dataset for CMIP6 and highl...
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with res...
We estimate the consequences of a potential strong decrease of the solar activity using the model si...
The role of stratospheric ozone changes in determining the climate response to solar forcing is inve...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
We investigate the effects of a recently proposed 21st century Dalton minimum like decline of solar ...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
During the 20th century, solar activity increased in magnitude to a so-called grand maximum. It is p...
We apply two reconstructed spectral solar forcing scenarios, one SIM (Spectral Irradiance Monitor) b...
The 11-year solar cycle forcing is recognised as a potentially important atmospheric forcing; howeve...
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with res...
The impact of changes in incoming solar irradiance on stratospheric ozone abundances should be inclu...
The 11 year solar‐cycle component of climate variability is assessed in historical simulations of mo...