Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean

The thermodynamic phase of clouds in low and middle levels over the Southern Ocean and the Arctic Ocean is poorly known, leading to uncertainties in the radiation budget in weather and climate models. To improve the knowledge of the cloud phase, we analyse two years of the raDAR-liDAR (DARDAR) datas...

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Main Authors: Dietel, Barbara, Sourdeval, Odran, Hoose, Corinna
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-2281
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2281/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere115238 2023-11-12T04:12:43+01:00 Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean Dietel, Barbara Sourdeval, Odran Hoose, Corinna 2023-10-12 application/pdf https://doi.org/10.5194/egusphere-2023-2281 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2281/ eng eng doi:10.5194/egusphere-2023-2281 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2281/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-2281 2023-10-16T16:24:15Z The thermodynamic phase of clouds in low and middle levels over the Southern Ocean and the Arctic Ocean is poorly known, leading to uncertainties in the radiation budget in weather and climate models. To improve the knowledge of the cloud phase, we analyse two years of the raDAR-liDAR (DARDAR) dataset based on active satellite instruments. We classify clouds according to their base and top height and focus on low-, mid- and mid-low-level clouds as they are most frequent in the mixed-phase temperature regime. Low-level single-layer clouds occur in 22–26 % of all profiles, but single-layer clouds spanning the mid-level also amount to approx. 15 %. Liquid clouds show mainly a smaller vertical extent, but a horizontally larger extent compared to ice clouds. The results show the highest liquid fractions for low-level and mid-level clouds. Two local minima in the liquid fraction are observed around cloud top temperatures of -15 °C and -5 °C. Mid-level and mid-low-level clouds over the Southern Ocean and low-level clouds in both polar regions show higher liquid fractions if they occur over sea ice compared to open ocean. Low-level clouds and mid-low-level clouds with high sea salt concentrations, used as a proxy for sea spray, show reduced liquid fractions. In mid-level clouds, dust shows the largest correlations with liquid fraction with a lower liquid fraction for a higher dust aerosol concentration. Low-level clouds clearly show the largest contribution to the shortwave cloud radiative effect in both polar regions followed by mid-low-level clouds. Text Arctic Arctic Ocean Sea ice Southern Ocean Copernicus Publications: E-Journals Arctic Southern Ocean Arctic Ocean
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The thermodynamic phase of clouds in low and middle levels over the Southern Ocean and the Arctic Ocean is poorly known, leading to uncertainties in the radiation budget in weather and climate models. To improve the knowledge of the cloud phase, we analyse two years of the raDAR-liDAR (DARDAR) dataset based on active satellite instruments. We classify clouds according to their base and top height and focus on low-, mid- and mid-low-level clouds as they are most frequent in the mixed-phase temperature regime. Low-level single-layer clouds occur in 22–26 % of all profiles, but single-layer clouds spanning the mid-level also amount to approx. 15 %. Liquid clouds show mainly a smaller vertical extent, but a horizontally larger extent compared to ice clouds. The results show the highest liquid fractions for low-level and mid-level clouds. Two local minima in the liquid fraction are observed around cloud top temperatures of -15 °C and -5 °C. Mid-level and mid-low-level clouds over the Southern Ocean and low-level clouds in both polar regions show higher liquid fractions if they occur over sea ice compared to open ocean. Low-level clouds and mid-low-level clouds with high sea salt concentrations, used as a proxy for sea spray, show reduced liquid fractions. In mid-level clouds, dust shows the largest correlations with liquid fraction with a lower liquid fraction for a higher dust aerosol concentration. Low-level clouds clearly show the largest contribution to the shortwave cloud radiative effect in both polar regions followed by mid-low-level clouds.
format Text
author Dietel, Barbara
Sourdeval, Odran
Hoose, Corinna
spellingShingle Dietel, Barbara
Sourdeval, Odran
Hoose, Corinna
Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
author_facet Dietel, Barbara
Sourdeval, Odran
Hoose, Corinna
author_sort Dietel, Barbara
title Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
title_short Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
title_full Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
title_fullStr Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
title_full_unstemmed Characterisation of low-base and mid-base clouds and their thermodynamic phase over the Southern and Arctic Ocean
title_sort characterisation of low-base and mid-base clouds and their thermodynamic phase over the southern and arctic ocean
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-2281
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2281/
geographic Arctic
Southern Ocean
Arctic Ocean
geographic_facet Arctic
Southern Ocean
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
Southern Ocean
genre_facet Arctic
Arctic Ocean
Sea ice
Southern Ocean
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-2281
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2281/
op_doi https://doi.org/10.5194/egusphere-2023-2281
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