Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)

The surface radiation environment over the Southern Ocean within the region bound by 42.8° S to 78.7° S and 62.6° E to 157.7° W is summarised for three austral summers. This is done using ship-based measurements with the combination of downwelling radiation sensors and a cloud imager. We focus on ch...

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Published in:Atmosphere
Main Authors: Haoran Wang, Andrew R. Klekociuk, W. John R. French, Simon P. Alexander, Tom A. Warner
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11090949
https://doaj.org/article/f5a1451584824038b176f1bbe34f9736
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spelling ftdoajarticles:oai:doaj.org/article:f5a1451584824038b176f1bbe34f9736 2023-05-15T18:07:33+02:00 Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E) Haoran Wang Andrew R. Klekociuk W. John R. French Simon P. Alexander Tom A. Warner 2020-09-01T00:00:00Z https://doi.org/10.3390/atmos11090949 https://doaj.org/article/f5a1451584824038b176f1bbe34f9736 EN eng MDPI AG https://www.mdpi.com/2073-4433/11/9/949 https://doaj.org/toc/2073-4433 doi:10.3390/atmos11090949 2073-4433 https://doaj.org/article/f5a1451584824038b176f1bbe34f9736 Atmosphere, Vol 11, Iss 949, p 949 (2020) Southern Ocean Ross Sea cloud shortwave radiation longwave radiation cloud radiative effect Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.3390/atmos11090949 2022-12-31T00:49:44Z The surface radiation environment over the Southern Ocean within the region bound by 42.8° S to 78.7° S and 62.6° E to 157.7° W is summarised for three austral summers. This is done using ship-based measurements with the combination of downwelling radiation sensors and a cloud imager. We focus on characterising the cloud radiative effect (CRE) under a variety of conditions, comparing observations in the open ocean with those in the sea ice zone. For comparison with our observed data, we obtained surface data from the European Centre for Medium-Range Weather Forecasts fifth reanalysis (ERA5). We found that the daily average cloud fraction was slightly lower in ERA5 compared with the observations (0.71 and 0.75, respectively). ERA5 also showed positive biases in the shortwave radiation effect and a negative bias in the longwave radiation effect. The observed mean surface CRE of −164 ± 100 Wm −2 was more negative than the mean surface CRE for ERA5 of −101 W m −2 . Article in Journal/Newspaper Ross Sea Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Southern Ocean Austral Ross Sea Atmosphere 11 9 949
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Southern Ocean
Ross Sea
cloud
shortwave radiation
longwave radiation
cloud radiative effect
Meteorology. Climatology
QC851-999
spellingShingle Southern Ocean
Ross Sea
cloud
shortwave radiation
longwave radiation
cloud radiative effect
Meteorology. Climatology
QC851-999
Haoran Wang
Andrew R. Klekociuk
W. John R. French
Simon P. Alexander
Tom A. Warner
Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
topic_facet Southern Ocean
Ross Sea
cloud
shortwave radiation
longwave radiation
cloud radiative effect
Meteorology. Climatology
QC851-999
description The surface radiation environment over the Southern Ocean within the region bound by 42.8° S to 78.7° S and 62.6° E to 157.7° W is summarised for three austral summers. This is done using ship-based measurements with the combination of downwelling radiation sensors and a cloud imager. We focus on characterising the cloud radiative effect (CRE) under a variety of conditions, comparing observations in the open ocean with those in the sea ice zone. For comparison with our observed data, we obtained surface data from the European Centre for Medium-Range Weather Forecasts fifth reanalysis (ERA5). We found that the daily average cloud fraction was slightly lower in ERA5 compared with the observations (0.71 and 0.75, respectively). ERA5 also showed positive biases in the shortwave radiation effect and a negative bias in the longwave radiation effect. The observed mean surface CRE of −164 ± 100 Wm −2 was more negative than the mean surface CRE for ERA5 of −101 W m −2 .
format Article in Journal/Newspaper
author Haoran Wang
Andrew R. Klekociuk
W. John R. French
Simon P. Alexander
Tom A. Warner
author_facet Haoran Wang
Andrew R. Klekociuk
W. John R. French
Simon P. Alexander
Tom A. Warner
author_sort Haoran Wang
title Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
title_short Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
title_full Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
title_fullStr Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
title_full_unstemmed Measurements of Cloud Radiative Effect across the Southern Ocean (43° S–79° S, 63° E–158° E)
title_sort measurements of cloud radiative effect across the southern ocean (43° s–79° s, 63° e–158° e)
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/atmos11090949
https://doaj.org/article/f5a1451584824038b176f1bbe34f9736
geographic Southern Ocean
Austral
Ross Sea
geographic_facet Southern Ocean
Austral
Ross Sea
genre Ross Sea
Sea ice
Southern Ocean
genre_facet Ross Sea
Sea ice
Southern Ocean
op_source Atmosphere, Vol 11, Iss 949, p 949 (2020)
op_relation https://www.mdpi.com/2073-4433/11/9/949
https://doaj.org/toc/2073-4433
doi:10.3390/atmos11090949
2073-4433
https://doaj.org/article/f5a1451584824038b176f1bbe34f9736
op_doi https://doi.org/10.3390/atmos11090949
container_title Atmosphere
container_volume 11
container_issue 9
container_start_page 949
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