Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign

<p>A large fraction of annual precipitation over the western United States comes from wintertime orographic clouds associated with atmospheric rivers (ARs). Transported African and Asian dust and marine aerosols from the Pacific Ocean may act as ice-nucleating particles (INPs) to affect cloud...

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Main Authors: Y. Lin, J. Fan, P. Li, L.-R. Leung, P. J. DeMott, L. Goldberger, J. Comstock, Y. Liu, J.-H. Jeong, J. Tomlinson
Format: Article
Language:English
Published: Copernicus Publications 2022-05-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/22/6749/2022/acp-22-6749-2022.pdf
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author Y. Lin
Y. Lin
J. Fan
P. Li
P. Li
L.-R. Leung
P. J. DeMott
L. Goldberger
J. Comstock
Y. Liu
J.-H. Jeong
J.-H. Jeong
J. Tomlinson
author_facet Y. Lin
Y. Lin
J. Fan
P. Li
P. Li
L.-R. Leung
P. J. DeMott
L. Goldberger
J. Comstock
Y. Liu
J.-H. Jeong
J.-H. Jeong
J. Tomlinson
author_sort Y. Lin
collection DOAJ
description <p>A large fraction of annual precipitation over the western United States comes from wintertime orographic clouds associated with atmospheric rivers (ARs). Transported African and Asian dust and marine aerosols from the Pacific Ocean may act as ice-nucleating particles (INPs) to affect cloud and precipitation properties over the region. Here we explored the effects of INPs from marine aerosols on orographic mixed-phase clouds and precipitation at different AR stages for an AR event observed during the 2015 ACAPEX field campaign under low dust (<span class="inline-formula"><i>&lt;</i>0.02</span> cm<span class="inline-formula"><sup>−3</sup></span>) conditions. Simulations were conducted using the chemistry version of the Weather Research and Forecasting Model coupled with the spectral-bin microphysics at 1 km grid spacing, with ice nucleation connected with dust and marine aerosols. By comparing against airborne and ground-based observations, accounting for marine INP effects improves the simulation of AR-precipitation. The marine INPs enhance the formation of ice and snow, leading to less shallow warm clouds but more mixed-phase and deep clouds, as well as to a large spillover effect of precipitation after AR landfall. The responses of cloud and precipitation to marine INPs vary with the AR stages, with more significant effects before AR landfall and post-AR than after AR landfall, mainly because the moisture and temperature conditions change with the AR evolution. This work suggests weather and climate models need to consider the impacts of marine INPs since their contribution is notable under low dust conditions despite the much lower relative ice nucleation efficiency of marine INPs.</p>
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spelling doaj.art-a9fdc1e05b744c69a075b4c6ef6eac452022-12-22T00:29:43ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242022-05-01226749677110.5194/acp-22-6749-2022Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaignY. Lin0Y. Lin1J. Fan2P. Li3P. Li4L.-R. Leung5P. J. DeMott6L. Goldberger7J. Comstock8Y. Liu9J.-H. Jeong10J.-H. Jeong11J. Tomlinson12Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USAJoint Institute for Regional Earth System Science and Engineering (JIFRESSE), University of California, Los Angeles (UCLA), Los Angeles, CA, 90064, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USACollege of Science and Technology, Hebei Agricultural University, Baoding, Hebei, 14 071000, PR ChinaResearch Center for Air Pollution and Health, Key Laboratory of Environmental Remediation and Ecological Health, Ministry of Education, College of Environment and Resource Sciences, Zhejiang University, Hangzhou, Zhejiang 310058, PR ChinaAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USADepartment of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USAJoint Institute for Regional Earth System Science and Engineering (JIFRESSE), University of California, Los Angeles (UCLA), Los Angeles, CA, 90064, USAAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA, 99352, USA<p>A large fraction of annual precipitation over the western United States comes from wintertime orographic clouds associated with atmospheric rivers (ARs). Transported African and Asian dust and marine aerosols from the Pacific Ocean may act as ice-nucleating particles (INPs) to affect cloud and precipitation properties over the region. Here we explored the effects of INPs from marine aerosols on orographic mixed-phase clouds and precipitation at different AR stages for an AR event observed during the 2015 ACAPEX field campaign under low dust (<span class="inline-formula"><i>&lt;</i>0.02</span> cm<span class="inline-formula"><sup>−3</sup></span>) conditions. Simulations were conducted using the chemistry version of the Weather Research and Forecasting Model coupled with the spectral-bin microphysics at 1 km grid spacing, with ice nucleation connected with dust and marine aerosols. By comparing against airborne and ground-based observations, accounting for marine INP effects improves the simulation of AR-precipitation. The marine INPs enhance the formation of ice and snow, leading to less shallow warm clouds but more mixed-phase and deep clouds, as well as to a large spillover effect of precipitation after AR landfall. The responses of cloud and precipitation to marine INPs vary with the AR stages, with more significant effects before AR landfall and post-AR than after AR landfall, mainly because the moisture and temperature conditions change with the AR evolution. This work suggests weather and climate models need to consider the impacts of marine INPs since their contribution is notable under low dust conditions despite the much lower relative ice nucleation efficiency of marine INPs.</p>https://acp.copernicus.org/articles/22/6749/2022/acp-22-6749-2022.pdf
spellingShingle Y. Lin
Y. Lin
J. Fan
P. Li
P. Li
L.-R. Leung
P. J. DeMott
L. Goldberger
J. Comstock
Y. Liu
J.-H. Jeong
J.-H. Jeong
J. Tomlinson
Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
Atmospheric Chemistry and Physics
title Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
title_full Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
title_fullStr Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
title_full_unstemmed Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
title_short Modeling impacts of ice-nucleating particles from marine aerosols on mixed-phase orographic clouds during 2015 ACAPEX field campaign
title_sort modeling impacts of ice nucleating particles from marine aerosols on mixed phase orographic clouds during 2015 acapex field campaign
url https://acp.copernicus.org/articles/22/6749/2022/acp-22-6749-2022.pdf
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