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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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 |
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Copernicus Publications: E-Journals |
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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 |
_version_ |
1766206410193895424 |