On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results

Using outputs from 10 CMIP5 models with fixed sea surface temperature, we investigate the fast response of the East Asian summer monsoon (EASM) and summer precipitation in East China to anthropogenic aerosols. To address this topic, we employ two commonly used EASM indices that can represent zonal a...

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Main Authors: Hongli Wang, Xiaoning Xie, Xiaodong Liu
Format: Article
Language:English
Published: Hindawi Limited 2015-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2015/397395
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spelling doaj-fb13812981c74b4caea54e5937268a772020-11-25T02:24:46ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172015-01-01201510.1155/2015/397395397395On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel ResultsHongli Wang0Xiaoning Xie1Xiaodong Liu2SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, ChinaSKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, ChinaSKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, ChinaUsing outputs from 10 CMIP5 models with fixed sea surface temperature, we investigate the fast response of the East Asian summer monsoon (EASM) and summer precipitation in East China to anthropogenic aerosols. To address this topic, we employ two commonly used EASM indices that can represent zonal and meridional land-sea thermal contrast, respectively. The results reveal that the notion of a weakened EASM in response to increased anthropogenic aerosols is a robust one, as well as decreased precipitation in East China. The ensemble mean of decreased precipitation in the aerosol run was about 6.6% in comparison to the CTL run and could be enlarged to 8.3% by excluding the experiments with the aerosol direct effect only. Convective precipitation was found to be the primary contributor (>80%) to the reduction of total precipitation. The combination of direct and indirect effects of aerosols can decrease solar radiation reaching the Earth’s surface and eventually modulate large-scale EASM circulation and suppress summer precipitation in East China. The uncertainties and discrepancies among the models highlight the complexity of interaction in aerosol-precipitation processes when investigating present and future changes of the EASM.http://dx.doi.org/10.1155/2015/397395
collection DOAJ
language English
format Article
sources DOAJ
author Hongli Wang
Xiaoning Xie
Xiaodong Liu
spellingShingle Hongli Wang
Xiaoning Xie
Xiaodong Liu
On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
Advances in Meteorology
author_facet Hongli Wang
Xiaoning Xie
Xiaodong Liu
author_sort Hongli Wang
title On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
title_short On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
title_full On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
title_fullStr On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
title_full_unstemmed On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results
title_sort on the robustness of the weakening effect of anthropogenic aerosols on the east asian summer monsoon with multimodel results
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2015-01-01
description Using outputs from 10 CMIP5 models with fixed sea surface temperature, we investigate the fast response of the East Asian summer monsoon (EASM) and summer precipitation in East China to anthropogenic aerosols. To address this topic, we employ two commonly used EASM indices that can represent zonal and meridional land-sea thermal contrast, respectively. The results reveal that the notion of a weakened EASM in response to increased anthropogenic aerosols is a robust one, as well as decreased precipitation in East China. The ensemble mean of decreased precipitation in the aerosol run was about 6.6% in comparison to the CTL run and could be enlarged to 8.3% by excluding the experiments with the aerosol direct effect only. Convective precipitation was found to be the primary contributor (>80%) to the reduction of total precipitation. The combination of direct and indirect effects of aerosols can decrease solar radiation reaching the Earth’s surface and eventually modulate large-scale EASM circulation and suppress summer precipitation in East China. The uncertainties and discrepancies among the models highlight the complexity of interaction in aerosol-precipitation processes when investigating present and future changes of the EASM.
url http://dx.doi.org/10.1155/2015/397395
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