Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO

The cloud amount, referred to as the frequency of cloud occurrences, is of great importance for the Earth–atmosphere system. It was conventionally quantified as the area fraction of clouds in a given region, discarding the three-dimensional nature of both cloud entities and their spatial distributio...

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Published in:Remote Sensing
Main Authors: Yuhao Ding, Qi Liu, Ping Lao, Meng Li, Yuan Li, Qun Zheng, Yanghui Peng
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15163978
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/16/3978/ 2023-09-05T13:19:55+02:00 Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO Yuhao Ding Qi Liu Ping Lao Meng Li Yuan Li Qun Zheng Yanghui Peng agris 2023-08-10 application/pdf https://doi.org/10.3390/rs15163978 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs15163978 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 16; Pages: 3978 cloud occurrences cloud volume fraction cloud types CloudSat CALIPSO Text 2023 ftmdpi https://doi.org/10.3390/rs15163978 2023-08-13T23:53:06Z The cloud amount, referred to as the frequency of cloud occurrences, is of great importance for the Earth–atmosphere system. It was conventionally quantified as the area fraction of clouds in a given region, discarding the three-dimensional nature of both cloud entities and their spatial distribution. Although the area fraction is explicit, it is the volume fraction that fully depicts cloud occurrences, and the area fraction is just related to a projection of the volume fraction. In this study, by using spaceborne radar measurements, the spatial distribution of cloud volume fraction throughout the troposphere was investigated, and the contributions of various cloud types at each location were clarified. Overall, the volume fraction of total clouds in the whole troposphere is 15.9%, while the corresponding area fraction relative to the global surface is 73.6%. The peak volume fraction occurs at 1 km altitude, mainly contributed by stratocumulus and cumulus. For a single cloud type, the maximum fraction is 48.8%, which is from stratocumulus and occurs at 1 km altitude above the Greenland Sea. Half of the eight cloud types, altostratus, cirrus, nimbostratus, and deep convective clouds, reach the nominal tropopause. In particular, the vertical distribution difference among multiple cloud types in each category (low-level, middle-level, and vertically extending) was clarified, and it was found that the dominant cloud type in a category varies notably with the location in the atmosphere. Text Greenland Greenland Sea MDPI Open Access Publishing Greenland Remote Sensing 15 16 3978
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic cloud occurrences
cloud volume fraction
cloud types
CloudSat
CALIPSO
spellingShingle cloud occurrences
cloud volume fraction
cloud types
CloudSat
CALIPSO
Yuhao Ding
Qi Liu
Ping Lao
Meng Li
Yuan Li
Qun Zheng
Yanghui Peng
Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
topic_facet cloud occurrences
cloud volume fraction
cloud types
CloudSat
CALIPSO
description The cloud amount, referred to as the frequency of cloud occurrences, is of great importance for the Earth–atmosphere system. It was conventionally quantified as the area fraction of clouds in a given region, discarding the three-dimensional nature of both cloud entities and their spatial distribution. Although the area fraction is explicit, it is the volume fraction that fully depicts cloud occurrences, and the area fraction is just related to a projection of the volume fraction. In this study, by using spaceborne radar measurements, the spatial distribution of cloud volume fraction throughout the troposphere was investigated, and the contributions of various cloud types at each location were clarified. Overall, the volume fraction of total clouds in the whole troposphere is 15.9%, while the corresponding area fraction relative to the global surface is 73.6%. The peak volume fraction occurs at 1 km altitude, mainly contributed by stratocumulus and cumulus. For a single cloud type, the maximum fraction is 48.8%, which is from stratocumulus and occurs at 1 km altitude above the Greenland Sea. Half of the eight cloud types, altostratus, cirrus, nimbostratus, and deep convective clouds, reach the nominal tropopause. In particular, the vertical distribution difference among multiple cloud types in each category (low-level, middle-level, and vertically extending) was clarified, and it was found that the dominant cloud type in a category varies notably with the location in the atmosphere.
format Text
author Yuhao Ding
Qi Liu
Ping Lao
Meng Li
Yuan Li
Qun Zheng
Yanghui Peng
author_facet Yuhao Ding
Qi Liu
Ping Lao
Meng Li
Yuan Li
Qun Zheng
Yanghui Peng
author_sort Yuhao Ding
title Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
title_short Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
title_full Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
title_fullStr Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
title_full_unstemmed Spatial Distributions of Cloud Occurrences in Terms of Volume Fraction as Inferred from CloudSat and CALIPSO
title_sort spatial distributions of cloud occurrences in terms of volume fraction as inferred from cloudsat and calipso
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15163978
op_coverage agris
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland Sea
genre_facet Greenland
Greenland Sea
op_source Remote Sensing; Volume 15; Issue 16; Pages: 3978
op_relation Atmospheric Remote Sensing
https://dx.doi.org/10.3390/rs15163978
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15163978
container_title Remote Sensing
container_volume 15
container_issue 16
container_start_page 3978
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