Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans

Abstract Aerosol effects on convective clouds and associated precipitation constitute an important open-ended question in climate research. Previous studies have linked an increase in aerosol concentration to a delay in the onset of rain, invigorated clouds and stronger rain rates. Here, using obser...

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Main Authors: Huan Liu, Jianping Guo, Ilan Koren, Orit Altaratz, Guy Dagan, Yuan Wang, Jonathan H. Jiang, Panmao Zhai, Yuk L. Yung
Format: Article
Language:English
Published: Nature Publishing Group 2019-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-019-44284-2
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spelling doaj-a87c1a03419c4f51a2805cc64a32fe232020-12-08T08:24:39ZengNature Publishing GroupScientific Reports2045-23222019-05-01911710.1038/s41598-019-44284-2Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical OceansHuan Liu0Jianping Guo1Ilan Koren2Orit Altaratz3Guy Dagan4Yuan Wang5Jonathan H. Jiang6Panmao Zhai7Yuk L. Yung8State Key Laboratory of Severe Weather, Chinese Academy of Meteorological SciencesState Key Laboratory of Severe Weather, Chinese Academy of Meteorological SciencesDepartment of Earth and Planetary Sciences, Weizmann Institute of ScienceDepartment of Earth and Planetary Sciences, Weizmann Institute of ScienceDepartment of Earth and Planetary Sciences, Weizmann Institute of ScienceDivision of Geological and Planetary Sciences, California Institute of TechnologyJet Propulsion Laboratory, California Institute of TechnologyState Key Laboratory of Severe Weather, Chinese Academy of Meteorological SciencesDivision of Geological and Planetary Sciences, California Institute of TechnologyAbstract Aerosol effects on convective clouds and associated precipitation constitute an important open-ended question in climate research. Previous studies have linked an increase in aerosol concentration to a delay in the onset of rain, invigorated clouds and stronger rain rates. Here, using observational data, we show that the aerosol effect on convective clouds shifts from invigoration to suppression with increasing aerosol optical depth. We explain this shift in trend (using a cloud model) as the result of a competition between two types of microphysical processes: cloud-core-based invigorating processes vs. peripheral suppressive processes. We show that the aerosol optical depth value that marks the shift between invigoration and suppression depends on the environmental thermodynamic conditions. These findings can aid in better parameterizing aerosol effects in climate models for the prediction of climate trends.https://doi.org/10.1038/s41598-019-44284-2
collection DOAJ
language English
format Article
sources DOAJ
author Huan Liu
Jianping Guo
Ilan Koren
Orit Altaratz
Guy Dagan
Yuan Wang
Jonathan H. Jiang
Panmao Zhai
Yuk L. Yung
spellingShingle Huan Liu
Jianping Guo
Ilan Koren
Orit Altaratz
Guy Dagan
Yuan Wang
Jonathan H. Jiang
Panmao Zhai
Yuk L. Yung
Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
Scientific Reports
author_facet Huan Liu
Jianping Guo
Ilan Koren
Orit Altaratz
Guy Dagan
Yuan Wang
Jonathan H. Jiang
Panmao Zhai
Yuk L. Yung
author_sort Huan Liu
title Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
title_short Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
title_full Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
title_fullStr Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
title_full_unstemmed Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans
title_sort non-monotonic aerosol effect on precipitation in convective clouds over tropical oceans
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2019-05-01
description Abstract Aerosol effects on convective clouds and associated precipitation constitute an important open-ended question in climate research. Previous studies have linked an increase in aerosol concentration to a delay in the onset of rain, invigorated clouds and stronger rain rates. Here, using observational data, we show that the aerosol effect on convective clouds shifts from invigoration to suppression with increasing aerosol optical depth. We explain this shift in trend (using a cloud model) as the result of a competition between two types of microphysical processes: cloud-core-based invigorating processes vs. peripheral suppressive processes. We show that the aerosol optical depth value that marks the shift between invigoration and suppression depends on the environmental thermodynamic conditions. These findings can aid in better parameterizing aerosol effects in climate models for the prediction of climate trends.
url https://doi.org/10.1038/s41598-019-44284-2
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