Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations

Drought is an extreme hydroclimate event that has been shown to cause the increase of surface fine dust near source regions, while the drought-dust relationship in regions predominantly influenced by long-range transported dust such as the southeastern US (SEUS) has received less attention. Using lo...

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Main Authors: Li, Wei, Wang, Yuxuan
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-18
https://noa.gwlb.de/receive/cop_mods_00060271
https://egusphere.copernicus.org/preprints/egusphere-2022-18/egusphere-2022-18.pdf
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00060271 2023-05-15T17:36:06+02:00 Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations Li, Wei Wang, Yuxuan 2022-02 electronic https://doi.org/10.5194/egusphere-2022-18 https://noa.gwlb.de/receive/cop_mods_00060271 https://egusphere.copernicus.org/preprints/egusphere-2022-18/egusphere-2022-18.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2022-18 https://noa.gwlb.de/receive/cop_mods_00060271 https://egusphere.copernicus.org/preprints/egusphere-2022-18/egusphere-2022-18.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/restrictedAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/egusphere-2022-18 2022-03-07T00:09:02Z Drought is an extreme hydroclimate event that has been shown to cause the increase of surface fine dust near source regions, while the drought-dust relationship in regions predominantly influenced by long-range transported dust such as the southeastern US (SEUS) has received less attention. Using long-term surface fine dust observations, weekly US Drought Monitor (USDM), and monthly Standardized Precipitation-Evapotranspiration Index (SPEI), this study unmasks spatial disparity in drought-dust relationships where the SEUS stands out as being abnormous in that it shows a decrease in surface dust concentrations during drought in contrast to the expected increase in dust found in other contiguous US (CONUS) regions. Surface fine dust was found to decrease by ~0.5 µg/m3 with a unit decrease of SPEI in the SEUS, as opposed to an increase of ~0.15 µg/m3 in the west. The anomalies of elemental ratios, satellite aerosol optical depth (AOD), and dust extinction coefficients suggest that both the emissions and trans-Atlantic transport of African dust are weakened when the SEUS is under droughts. Through the teleconnection patterns of negative North Atlantic Oscillation (NAO), a lower than normal and more northeastward displacement of the Bermuda High (BH) was present during SEUS droughts which resulted in less dust being transported into the SEUS. At the same time, enhanced precipitation in Sahel associated with the northward shift of the Intertropical Convergence Zone (ITCZ) leads to lower dust emissions therein. Of the four selected models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6), GISS-E2-1-G was found to perform the best in capturing the drought-dust sensitivity in the SEUS. This study reveals the mechanism of how regional-scale droughts influence aerosol abundance through changing long-range transport of dust. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Niedersächsisches Online-Archiv NOA
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Li, Wei
Wang, Yuxuan
Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
topic_facet article
Verlagsveröffentlichung
description Drought is an extreme hydroclimate event that has been shown to cause the increase of surface fine dust near source regions, while the drought-dust relationship in regions predominantly influenced by long-range transported dust such as the southeastern US (SEUS) has received less attention. Using long-term surface fine dust observations, weekly US Drought Monitor (USDM), and monthly Standardized Precipitation-Evapotranspiration Index (SPEI), this study unmasks spatial disparity in drought-dust relationships where the SEUS stands out as being abnormous in that it shows a decrease in surface dust concentrations during drought in contrast to the expected increase in dust found in other contiguous US (CONUS) regions. Surface fine dust was found to decrease by ~0.5 µg/m3 with a unit decrease of SPEI in the SEUS, as opposed to an increase of ~0.15 µg/m3 in the west. The anomalies of elemental ratios, satellite aerosol optical depth (AOD), and dust extinction coefficients suggest that both the emissions and trans-Atlantic transport of African dust are weakened when the SEUS is under droughts. Through the teleconnection patterns of negative North Atlantic Oscillation (NAO), a lower than normal and more northeastward displacement of the Bermuda High (BH) was present during SEUS droughts which resulted in less dust being transported into the SEUS. At the same time, enhanced precipitation in Sahel associated with the northward shift of the Intertropical Convergence Zone (ITCZ) leads to lower dust emissions therein. Of the four selected models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6), GISS-E2-1-G was found to perform the best in capturing the drought-dust sensitivity in the SEUS. This study reveals the mechanism of how regional-scale droughts influence aerosol abundance through changing long-range transport of dust.
format Article in Journal/Newspaper
author Li, Wei
Wang, Yuxuan
author_facet Li, Wei
Wang, Yuxuan
author_sort Li, Wei
title Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
title_short Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
title_full Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
title_fullStr Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
title_full_unstemmed Reduced surface fine dust under droughts over the southeastern United States during summertime: observations and CMIP6 model simulations
title_sort reduced surface fine dust under droughts over the southeastern united states during summertime: observations and cmip6 model simulations
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/egusphere-2022-18
https://noa.gwlb.de/receive/cop_mods_00060271
https://egusphere.copernicus.org/preprints/egusphere-2022-18/egusphere-2022-18.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://doi.org/10.5194/egusphere-2022-18
https://noa.gwlb.de/receive/cop_mods_00060271
https://egusphere.copernicus.org/preprints/egusphere-2022-18/egusphere-2022-18.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/restrictedAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/egusphere-2022-18
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