Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8

The cool skin effect refers to the phenomenon where the surface skin temperature of the ocean is always slightly cooler than the temperature of the water directly underneath due to the ubiquitous cooling processes at the ocean surface, especially in the absence of solar radiation. The cool skin effe...

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Published in:Remote Sensing
Main Authors: Yueqi Zhang, Zhaohui Chen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15184408
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/18/4408/ 2023-10-09T21:56:03+02:00 Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8 Yueqi Zhang Zhaohui Chen agris 2023-09-07 application/pdf https://doi.org/10.3390/rs15184408 eng eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs15184408 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 15 Issue 18 Pages: 4408 cool skin effect geostationary satellite carbon dioxide flux air–sea interaction Text 2023 ftmdpi https://doi.org/10.3390/rs15184408 2023-09-10T23:54:59Z The cool skin effect refers to the phenomenon where the surface skin temperature of the ocean is always slightly cooler than the temperature of the water directly underneath due to the ubiquitous cooling processes at the ocean surface, especially in the absence of solar radiation. The cool skin effect plays a critical role in the estimation of heat, momentum, and gas exchange between the air and the sea. However, the scarcity of observational data greatly hinders the accurate assessment of the cool skin effect. Here, the matchup data from the new generation geostationary satellite Himawari-8 and in situ sea surface temperature (SST) observations are used to evaluate the performance and dependence on the cool skin effect in the low/mid-latitude oceans. Results show that the intensity of the cool skin effect as revealed by Himawari-8 (−0.16 K) is found to be relatively weaker than previously published cool skin models based on in situ concurrent observations. A considerable amount of warm skin signals has been detected in the high-latitude oceans (e.g., Southern Ocean) under the circumstances of positive air–sea temperature difference and high wind, which may be the main cause of discrepancies with previous thoughts on the cool skin effect. Text Southern Ocean MDPI Open Access Publishing Southern Ocean Remote Sensing 15 18 4408
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic cool skin effect
geostationary satellite
carbon dioxide flux
air–sea interaction
spellingShingle cool skin effect
geostationary satellite
carbon dioxide flux
air–sea interaction
Yueqi Zhang
Zhaohui Chen
Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
topic_facet cool skin effect
geostationary satellite
carbon dioxide flux
air–sea interaction
description The cool skin effect refers to the phenomenon where the surface skin temperature of the ocean is always slightly cooler than the temperature of the water directly underneath due to the ubiquitous cooling processes at the ocean surface, especially in the absence of solar radiation. The cool skin effect plays a critical role in the estimation of heat, momentum, and gas exchange between the air and the sea. However, the scarcity of observational data greatly hinders the accurate assessment of the cool skin effect. Here, the matchup data from the new generation geostationary satellite Himawari-8 and in situ sea surface temperature (SST) observations are used to evaluate the performance and dependence on the cool skin effect in the low/mid-latitude oceans. Results show that the intensity of the cool skin effect as revealed by Himawari-8 (−0.16 K) is found to be relatively weaker than previously published cool skin models based on in situ concurrent observations. A considerable amount of warm skin signals has been detected in the high-latitude oceans (e.g., Southern Ocean) under the circumstances of positive air–sea temperature difference and high wind, which may be the main cause of discrepancies with previous thoughts on the cool skin effect.
format Text
author Yueqi Zhang
Zhaohui Chen
author_facet Yueqi Zhang
Zhaohui Chen
author_sort Yueqi Zhang
title Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
title_short Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
title_full Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
title_fullStr Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
title_full_unstemmed Cool Skin Effect as Seen from a New Generation Geostationary Satellite Himawari-8
title_sort cool skin effect as seen from a new generation geostationary satellite himawari-8
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15184408
op_coverage agris
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source Remote Sensing
Volume 15
Issue 18
Pages: 4408
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs15184408
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15184408
container_title Remote Sensing
container_volume 15
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