Cloud properties over the Southern Ocean during the MARCUS field campaign

To investigate the cloud properties over the Southern Ocean (SO), the MARCUS field campaign (41 to 69º S; 60 to 160º E) was conducted from October 2017 to March 2018, using ship-based measurements. To examine cloud properties over the mid-latitude and Polar regions, the study domain is separated int...

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Main Authors: Xi, Baike, Dong, Xiquan, Zheng, Xiaojian, Wu, Peng
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/amt-2021-388
https://amt.copernicus.org/preprints/amt-2021-388/
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spelling ftcopernicus:oai:publications.copernicus.org:amtd99136 2023-05-15T18:25:10+02:00 Cloud properties over the Southern Ocean during the MARCUS field campaign Xi, Baike Dong, Xiquan Zheng, Xiaojian Wu, Peng 2022-01-17 application/pdf https://doi.org/10.5194/amt-2021-388 https://amt.copernicus.org/preprints/amt-2021-388/ eng eng doi:10.5194/amt-2021-388 https://amt.copernicus.org/preprints/amt-2021-388/ eISSN: 1867-8548 Text 2022 ftcopernicus https://doi.org/10.5194/amt-2021-388 2022-01-24T17:22:18Z To investigate the cloud properties over the Southern Ocean (SO), the MARCUS field campaign (41 to 69º S; 60 to 160º E) was conducted from October 2017 to March 2018, using ship-based measurements. To examine cloud properties over the mid-latitude and Polar regions, the study domain is separated into northern (NSO) and southern (SSO) parts of the SO with a demarcation line of 60° S. The total cloud fractions ( CF s) were 77.9 %, 67.6 %, and 90.3 % for the entire domain, NSO and SSO, respectively, indicating that higher CFs were observed in the Polar region. Low-level clouds, deep cumulus, and shallow cumulus clouds are the three most common cloud types over the SO. For single-layered low-level clouds, mixed-phase clouds dominate with an occurrence frequency ( Freq ) of 54.5 %, while the Freq of the liquid and ice clouds were 10.1 % (most drizzling) and 17.4 % (least drizzling). The meridional distributions of low-level cloud boundaries are nearly independent of latitude, whereas the cloud temperatures increased ~ 8 K and atmospheric precipitable water vapor increased from ~5 mm at 69º S to ~18 mm at 43º S. The mean cloud liquid water paths over NSO were much larger than those over SSO. Most liquid clouds occurred over NSO with very few over SSO, whereas more mixed-phase clouds occurred over SSO than over NSO. There were no significant differences for ice cloud Freq between NSO and SSO. These results will be valuable for advancing our understanding of the meridional and vertical distributions of clouds and can be used to improve model simulations over the SO. Text Southern Ocean Copernicus Publications: E-Journals Southern Ocean
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description To investigate the cloud properties over the Southern Ocean (SO), the MARCUS field campaign (41 to 69º S; 60 to 160º E) was conducted from October 2017 to March 2018, using ship-based measurements. To examine cloud properties over the mid-latitude and Polar regions, the study domain is separated into northern (NSO) and southern (SSO) parts of the SO with a demarcation line of 60° S. The total cloud fractions ( CF s) were 77.9 %, 67.6 %, and 90.3 % for the entire domain, NSO and SSO, respectively, indicating that higher CFs were observed in the Polar region. Low-level clouds, deep cumulus, and shallow cumulus clouds are the three most common cloud types over the SO. For single-layered low-level clouds, mixed-phase clouds dominate with an occurrence frequency ( Freq ) of 54.5 %, while the Freq of the liquid and ice clouds were 10.1 % (most drizzling) and 17.4 % (least drizzling). The meridional distributions of low-level cloud boundaries are nearly independent of latitude, whereas the cloud temperatures increased ~ 8 K and atmospheric precipitable water vapor increased from ~5 mm at 69º S to ~18 mm at 43º S. The mean cloud liquid water paths over NSO were much larger than those over SSO. Most liquid clouds occurred over NSO with very few over SSO, whereas more mixed-phase clouds occurred over SSO than over NSO. There were no significant differences for ice cloud Freq between NSO and SSO. These results will be valuable for advancing our understanding of the meridional and vertical distributions of clouds and can be used to improve model simulations over the SO.
format Text
author Xi, Baike
Dong, Xiquan
Zheng, Xiaojian
Wu, Peng
spellingShingle Xi, Baike
Dong, Xiquan
Zheng, Xiaojian
Wu, Peng
Cloud properties over the Southern Ocean during the MARCUS field campaign
author_facet Xi, Baike
Dong, Xiquan
Zheng, Xiaojian
Wu, Peng
author_sort Xi, Baike
title Cloud properties over the Southern Ocean during the MARCUS field campaign
title_short Cloud properties over the Southern Ocean during the MARCUS field campaign
title_full Cloud properties over the Southern Ocean during the MARCUS field campaign
title_fullStr Cloud properties over the Southern Ocean during the MARCUS field campaign
title_full_unstemmed Cloud properties over the Southern Ocean during the MARCUS field campaign
title_sort cloud properties over the southern ocean during the marcus field campaign
publishDate 2022
url https://doi.org/10.5194/amt-2021-388
https://amt.copernicus.org/preprints/amt-2021-388/
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-2021-388
https://amt.copernicus.org/preprints/amt-2021-388/
op_doi https://doi.org/10.5194/amt-2021-388
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