Natural marine cloud brightening in the Southern Ocean

The number of cloud droplets per unit volume (N d ) is a fundamentally important property of marine boundary layer (MBL) liquid clouds that, at constant liquid water path, exerts considerable controls on albedo. Past work has shown that regional N d has a direct correlation to marine primary product...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Mace, Gerald G., Benson, Sally, Humphries, Ruhi, Gombert, Peter M., Sterner, Elizabeth
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1958432
https://www.osti.gov/biblio/1958432
https://doi.org/10.5194/acp-23-1677-2023
id ftosti:oai:osti.gov:1958432
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spelling ftosti:oai:osti.gov:1958432 2023-07-30T03:57:43+02:00 Natural marine cloud brightening in the Southern Ocean Mace, Gerald G. Benson, Sally Humphries, Ruhi Gombert, Peter M. Sterner, Elizabeth 2023-03-06 application/pdf http://www.osti.gov/servlets/purl/1958432 https://www.osti.gov/biblio/1958432 https://doi.org/10.5194/acp-23-1677-2023 unknown http://www.osti.gov/servlets/purl/1958432 https://www.osti.gov/biblio/1958432 https://doi.org/10.5194/acp-23-1677-2023 doi:10.5194/acp-23-1677-2023 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.5194/acp-23-1677-2023 2023-07-11T10:24:54Z The number of cloud droplets per unit volume (N d ) is a fundamentally important property of marine boundary layer (MBL) liquid clouds that, at constant liquid water path, exerts considerable controls on albedo. Past work has shown that regional N d has a direct correlation to marine primary productivity (PP) because of the role of seasonally varying, biogenically derived precursor gases in modulating secondary aerosol properties. These linkages are thought to be observable over the high-latitude oceans, where strong seasonal variability in aerosol and meteorology covary in mostly pristine environments. Here, we examine N d variability derived from 5 years of MODIS Level 2-derived cloud properties in a broad region of the summer eastern Southern Ocean and adjacent marginal seas. We demonstrate latitudinal, longitudinal and temporal gradients in N d that are strongly correlated with the passage of air masses over high-PP waters that are mostly concentrated along the Antarctic Shelf poleward of 60°S. We find that the albedo of MBL clouds in the latitudes south of 60°S is significantly higher than similar liquid water path (LWP) clouds north of this latitude. Other/Unknown Material Antarc* Antarctic Southern Ocean SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Antarctic Southern Ocean The Antarctic Atmospheric Chemistry and Physics 23 2 1677 1685
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Mace, Gerald G.
Benson, Sally
Humphries, Ruhi
Gombert, Peter M.
Sterner, Elizabeth
Natural marine cloud brightening in the Southern Ocean
topic_facet 54 ENVIRONMENTAL SCIENCES
description The number of cloud droplets per unit volume (N d ) is a fundamentally important property of marine boundary layer (MBL) liquid clouds that, at constant liquid water path, exerts considerable controls on albedo. Past work has shown that regional N d has a direct correlation to marine primary productivity (PP) because of the role of seasonally varying, biogenically derived precursor gases in modulating secondary aerosol properties. These linkages are thought to be observable over the high-latitude oceans, where strong seasonal variability in aerosol and meteorology covary in mostly pristine environments. Here, we examine N d variability derived from 5 years of MODIS Level 2-derived cloud properties in a broad region of the summer eastern Southern Ocean and adjacent marginal seas. We demonstrate latitudinal, longitudinal and temporal gradients in N d that are strongly correlated with the passage of air masses over high-PP waters that are mostly concentrated along the Antarctic Shelf poleward of 60°S. We find that the albedo of MBL clouds in the latitudes south of 60°S is significantly higher than similar liquid water path (LWP) clouds north of this latitude.
author Mace, Gerald G.
Benson, Sally
Humphries, Ruhi
Gombert, Peter M.
Sterner, Elizabeth
author_facet Mace, Gerald G.
Benson, Sally
Humphries, Ruhi
Gombert, Peter M.
Sterner, Elizabeth
author_sort Mace, Gerald G.
title Natural marine cloud brightening in the Southern Ocean
title_short Natural marine cloud brightening in the Southern Ocean
title_full Natural marine cloud brightening in the Southern Ocean
title_fullStr Natural marine cloud brightening in the Southern Ocean
title_full_unstemmed Natural marine cloud brightening in the Southern Ocean
title_sort natural marine cloud brightening in the southern ocean
publishDate 2023
url http://www.osti.gov/servlets/purl/1958432
https://www.osti.gov/biblio/1958432
https://doi.org/10.5194/acp-23-1677-2023
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation http://www.osti.gov/servlets/purl/1958432
https://www.osti.gov/biblio/1958432
https://doi.org/10.5194/acp-23-1677-2023
doi:10.5194/acp-23-1677-2023
op_doi https://doi.org/10.5194/acp-23-1677-2023
container_title Atmospheric Chemistry and Physics
container_volume 23
container_issue 2
container_start_page 1677
op_container_end_page 1685
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