Articles | Volume 21, issue 13
https://doi.org/10.5194/acp-21-10179-2021
https://doi.org/10.5194/acp-21-10179-2021
Research article
 | 
07 Jul 2021
Research article |  | 07 Jul 2021

On the contribution of fast and slow responses to precipitation changes caused by aerosol perturbations

Shipeng Zhang, Philip Stier, and Duncan Watson-Parris

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Cited articles

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Ackerman, A. S., Kirkpatrick, M. P., Stevens, D. E., and Toon, O. B.: The impact of humidity above stratiform clouds on indirect aerosol climate forcing, Nature, 432, 1014–1017, https://doi.org/10.1038/nature03174, 2004. 
Alizadeh-Choobari, O.: Impact of aerosol number concentration on precipitation under different precipitation rates, Meteorol. Appl., 25, 596–605, https://doi.org/10.1002/met.1724, 2018. 
Allen, M. R. and Ingram, W. J.: Constraints on future changes in climate and the hydrologic cycle, Nature, 419, 228–232, https://doi.org/10.1038/nature01092, 2002. 
Andrews, T., Forster, P. M., and Gregory, J. M.: A surface energy perspective on climate change, J. Climate, 22, 2557–2570, https://doi.org/10.1175/2008JCLI2759.1, 2009. 
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The relationship between aerosol-induced changes in atmospheric energetics and precipitation responses across different scales is studied in terms of fast (radiatively or microphysically mediated) and slow (temperature-mediated) responses. We introduced a method to decompose rainfall changes into contributions from clouds, aerosols, and clear–clean sky from an energetic perspective. It provides a way to better interpret and quantify the precipitation changes caused by aerosol perturbations.
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