Articles | Volume 18, issue 8
https://doi.org/10.5194/acp-18-5821-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-5821-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 Apr 2018
Research article |
| 26 Apr 2018
| 26 Apr 2018
Aerosol midlatitude cyclone indirect effects in observations and high-resolution simulations
School of Earth and Environment, Institute of Climate and Atmospheric
Science, University of Leeds, Leeds, LS2 9JT, UK
Paul R. Field
School of Earth and Environment, Institute of Climate and Atmospheric
Science, University of Leeds, Leeds, LS2 9JT, UK
Met Office, Fitzroy Rd, Exeter EX1 3PB, UK
Anja Schmidt
School of Earth and Environment, Institute of Climate and Atmospheric
Science, University of Leeds, Leeds, LS2 9JT, UK
Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW,
UK
Department of Geography, University of Cambridge, Downing Place,
Cambridge CB2 3EN, UK
Daniel P. Grosvenor
School of Earth and Environment, Institute of Climate and Atmospheric
Science, University of Leeds, Leeds, LS2 9JT, UK
National Centre for Atmospheric Science (NCAS), University of Leeds,
Leeds, LS2 9JT, UK
Frida A.-M. Bender
Department of Meteorology and Bolin Centre for Climate Research,
Stockholm University, Stockholm, 106 91, Sweden
Ben J. Shipway
Met Office, Fitzroy Rd, Exeter EX1 3PB, UK
Adrian A. Hill
Met Office, Fitzroy Rd, Exeter EX1 3PB, UK
Jonathan M. Wilkinson
Met Office, Fitzroy Rd, Exeter EX1 3PB, UK
Gregory S. Elsaesser
Department of Applied Physics and Applied Mathematics, Columbia
University and NASA Goddard Institute for Space Studies, New York, NY, USA
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Short summary
Here we use a combination of global convection-permitting models, satellite observations and the Holuhraun volcanic eruption to demonstrate that aerosol enhances the cloud liquid content and brightness of midlatitude cyclones. This is important because the strength of anthropogenic radiative forcing is uncertain, leading to uncertainty in the climate sensitivity consistent with observed temperature record.
Here we use a combination of global convection-permitting models, satellite observations and the...
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