Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations

The supercooled liquid fraction (SLF) in mixed-phase clouds (MPCs) is an essential variable of cloud microphysical processes and climate sensitivity. However, the SLF is currently calculated in spaceborne remote sensing only as the cloud phase–frequency ratio of adjacent pixels, which results in a l...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Wang, Ziming, Letu, Husi, Shang, Huazhe, Bugliaro, Luca
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/acp-24-7559-2024
https://acp.copernicus.org/articles/24/7559/2024/
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spelling ftcopernicus:oai:publications.copernicus.org:acp115930 2024-09-15T18:37:20+00:00 Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations Wang, Ziming Letu, Husi Shang, Huazhe Bugliaro, Luca 2024-07-04 application/pdf https://doi.org/10.5194/acp-24-7559-2024 https://acp.copernicus.org/articles/24/7559/2024/ eng eng doi:10.5194/acp-24-7559-2024 https://acp.copernicus.org/articles/24/7559/2024/ eISSN: 1680-7324 Text 2024 ftcopernicus https://doi.org/10.5194/acp-24-7559-2024 2024-08-28T05:24:22Z The supercooled liquid fraction (SLF) in mixed-phase clouds (MPCs) is an essential variable of cloud microphysical processes and climate sensitivity. However, the SLF is currently calculated in spaceborne remote sensing only as the cloud phase–frequency ratio of adjacent pixels, which results in a loss of the original resolution in observations of cloud liquid or ice content within MPCs. Here, we present a novel method for retrieving the SLF in MPCs based on the differences in radiative properties of supercooled liquid droplets and ice particles at visible (VIS) and shortwave infrared (SWI) channels of the geostationary Himawari-8. Liquid and ice water paths are inferred by assuming that clouds are composed of only liquid or ice, with the real cloud water path (CWP) expressed as a combination of these two water paths (SLF and 1-SLF as coefficients), and the SLF is determined by referring to the CWP from Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO). The statistically relatively small cloud phase spatial inhomogeneity at a Himawari-8 pixel level indicates an optimal scene for cloud retrieval. The SLF results are comparable to global SLF distributions observed by active instruments, particularly for single-layered cloud systems. While accessing the method's feasibility, SLF averages are estimated between 74 % and 78 % in Southern Ocean (SO) stratocumulus across seasons, contrasting with a range of 29 % to 32 % in northeastern Asia. The former exhibits a minimum SLF around midday in summer and a maximum in winter, while the latter trend differs. This novel algorithm will be valuable for research to track the evolution of MPCs and constrain the related climate impact. Text Southern Ocean Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 24 13 7559 7574
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The supercooled liquid fraction (SLF) in mixed-phase clouds (MPCs) is an essential variable of cloud microphysical processes and climate sensitivity. However, the SLF is currently calculated in spaceborne remote sensing only as the cloud phase–frequency ratio of adjacent pixels, which results in a loss of the original resolution in observations of cloud liquid or ice content within MPCs. Here, we present a novel method for retrieving the SLF in MPCs based on the differences in radiative properties of supercooled liquid droplets and ice particles at visible (VIS) and shortwave infrared (SWI) channels of the geostationary Himawari-8. Liquid and ice water paths are inferred by assuming that clouds are composed of only liquid or ice, with the real cloud water path (CWP) expressed as a combination of these two water paths (SLF and 1-SLF as coefficients), and the SLF is determined by referring to the CWP from Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO). The statistically relatively small cloud phase spatial inhomogeneity at a Himawari-8 pixel level indicates an optimal scene for cloud retrieval. The SLF results are comparable to global SLF distributions observed by active instruments, particularly for single-layered cloud systems. While accessing the method's feasibility, SLF averages are estimated between 74 % and 78 % in Southern Ocean (SO) stratocumulus across seasons, contrasting with a range of 29 % to 32 % in northeastern Asia. The former exhibits a minimum SLF around midday in summer and a maximum in winter, while the latter trend differs. This novel algorithm will be valuable for research to track the evolution of MPCs and constrain the related climate impact.
format Text
author Wang, Ziming
Letu, Husi
Shang, Huazhe
Bugliaro, Luca
spellingShingle Wang, Ziming
Letu, Husi
Shang, Huazhe
Bugliaro, Luca
Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
author_facet Wang, Ziming
Letu, Husi
Shang, Huazhe
Bugliaro, Luca
author_sort Wang, Ziming
title Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
title_short Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
title_full Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
title_fullStr Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
title_full_unstemmed Technical note: Retrieval of the supercooled liquid fraction in mixed-phase clouds from Himawari-8 observations
title_sort technical note: retrieval of the supercooled liquid fraction in mixed-phase clouds from himawari-8 observations
publishDate 2024
url https://doi.org/10.5194/acp-24-7559-2024
https://acp.copernicus.org/articles/24/7559/2024/
genre Southern Ocean
genre_facet Southern Ocean
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-24-7559-2024
https://acp.copernicus.org/articles/24/7559/2024/
op_doi https://doi.org/10.5194/acp-24-7559-2024
container_title Atmospheric Chemistry and Physics
container_volume 24
container_issue 13
container_start_page 7559
op_container_end_page 7574
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