Articles | Volume 19, issue 8
https://doi.org/10.5194/acp-19-5331-2019
© Author(s) 2019. 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-19-5331-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
18 Apr 2019
Research article |
| 18 Apr 2019
| 18 Apr 2019
Constraining the aerosol influence on cloud liquid water path
Edward Gryspeerdt
CORRESPONDING AUTHOR
Space and Atmospheric Physics Group, Imperial College, London, UK
Tom Goren
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Odran Sourdeval
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Laboratoire d'Optique Atmosphérique, Université de Lille, Villeneuve-d'Ascq, France
Johannes Quaas
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Johannes Mülmenstädt
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Sudhakar Dipu
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Claudia Unglaub
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Andrew Gettelman
National Center for Atmospheric Research, Boulder, CO, USA
Matthew Christensen
Department of Physics, University of Oxford, Oxford, UK
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Latest update: 20 Nov 2024
Short summary
The liquid water path (LWP) is the strongest control on cloud albedo, such that a small change in LWP can have a large radiative impact. By changing the droplet number concentration (Nd) aerosols may be able to change the LWP, but the sign and magnitude of the effect is unclear. This work uses satellite data to investigate the relationship between Nd and LWP at a global scale and in response to large aerosol perturbations, suggesting that a strong decrease in LWP at high Nd may be overestimated.
The liquid water path (LWP) is the strongest control on cloud albedo, such that a small change...
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