Variations in the Upper Ocean Heat Content of the Southern Canadian Basin

The marine environment of the Arctic Ocean has changed rapidly in recent decades. We used reanalysis data and observational data to explore the variations in the upper ocean heat content (OHC) of the Canadian Basin (CB) and the variations in the temperature profiles of the Southern Canadian Basin (S...

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Published in:Journal of Marine Science and Engineering
Main Authors: Yu Liu, Changcheng Ye, Haobin Cen, Xiayan Lin, Guoqing Han
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2024
Subjects:
Online Access:https://doi.org/10.3390/jmse12040667
https://doaj.org/article/cfa7fa87cd9b47bfa21e2766301b963d
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spelling ftdoajarticles:oai:doaj.org/article:cfa7fa87cd9b47bfa21e2766301b963d 2024-09-15T17:53:56+00:00 Variations in the Upper Ocean Heat Content of the Southern Canadian Basin Yu Liu Changcheng Ye Haobin Cen Xiayan Lin Guoqing Han 2024-04-01T00:00:00Z https://doi.org/10.3390/jmse12040667 https://doaj.org/article/cfa7fa87cd9b47bfa21e2766301b963d EN eng MDPI AG https://www.mdpi.com/2077-1312/12/4/667 https://doaj.org/toc/2077-1312 doi:10.3390/jmse12040667 2077-1312 https://doaj.org/article/cfa7fa87cd9b47bfa21e2766301b963d Journal of Marine Science and Engineering, Vol 12, Iss 4, p 667 (2024) Canadian Basin ocean heat content temperature profile Pacific warm water Atlantic warm water Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 article 2024 ftdoajarticles https://doi.org/10.3390/jmse12040667 2024-08-05T17:49:32Z The marine environment of the Arctic Ocean has changed rapidly in recent decades. We used reanalysis data and observational data to explore the variations in the upper ocean heat content (OHC) of the Canadian Basin (CB) and the variations in the temperature profiles of the Southern Canadian Basin (SCB). Both the reanalysis data and observational data show increasing trends for the OHC of the CB from 1993 to 2023. Compared to the World Ocean Atlas data (WOA 18/23), the reanalysis data (ORAS5 or GLORYS12V1) significantly underestimated the values of the upper OHC of the Canadian Basin. To explain the OHC differences, the Ice-Tethered Profiler (ITP) observational data were used to analyze the variations in the vertical temperature profiles. We found that the reanalysis data remarkably underestimated the maximum temperatures of the subsurface Pacific warm water and its increasing trend. Based on the short-term prediction results from the Bi-LSTM neural network, we forecasted that the upper OHC will continue to increase in the SCB, mainly due to the warming of the intermediate Atlantic warm water. The research results provide a valuable reference for assessing and improving climate-coupled models. Article in Journal/Newspaper Arctic Ocean Directory of Open Access Journals: DOAJ Articles Journal of Marine Science and Engineering 12 4 667
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Canadian Basin
ocean heat content
temperature profile
Pacific warm water
Atlantic warm water
Naval architecture. Shipbuilding. Marine engineering
VM1-989
Oceanography
GC1-1581
spellingShingle Canadian Basin
ocean heat content
temperature profile
Pacific warm water
Atlantic warm water
Naval architecture. Shipbuilding. Marine engineering
VM1-989
Oceanography
GC1-1581
Yu Liu
Changcheng Ye
Haobin Cen
Xiayan Lin
Guoqing Han
Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
topic_facet Canadian Basin
ocean heat content
temperature profile
Pacific warm water
Atlantic warm water
Naval architecture. Shipbuilding. Marine engineering
VM1-989
Oceanography
GC1-1581
description The marine environment of the Arctic Ocean has changed rapidly in recent decades. We used reanalysis data and observational data to explore the variations in the upper ocean heat content (OHC) of the Canadian Basin (CB) and the variations in the temperature profiles of the Southern Canadian Basin (SCB). Both the reanalysis data and observational data show increasing trends for the OHC of the CB from 1993 to 2023. Compared to the World Ocean Atlas data (WOA 18/23), the reanalysis data (ORAS5 or GLORYS12V1) significantly underestimated the values of the upper OHC of the Canadian Basin. To explain the OHC differences, the Ice-Tethered Profiler (ITP) observational data were used to analyze the variations in the vertical temperature profiles. We found that the reanalysis data remarkably underestimated the maximum temperatures of the subsurface Pacific warm water and its increasing trend. Based on the short-term prediction results from the Bi-LSTM neural network, we forecasted that the upper OHC will continue to increase in the SCB, mainly due to the warming of the intermediate Atlantic warm water. The research results provide a valuable reference for assessing and improving climate-coupled models.
format Article in Journal/Newspaper
author Yu Liu
Changcheng Ye
Haobin Cen
Xiayan Lin
Guoqing Han
author_facet Yu Liu
Changcheng Ye
Haobin Cen
Xiayan Lin
Guoqing Han
author_sort Yu Liu
title Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
title_short Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
title_full Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
title_fullStr Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
title_full_unstemmed Variations in the Upper Ocean Heat Content of the Southern Canadian Basin
title_sort variations in the upper ocean heat content of the southern canadian basin
publisher MDPI AG
publishDate 2024
url https://doi.org/10.3390/jmse12040667
https://doaj.org/article/cfa7fa87cd9b47bfa21e2766301b963d
genre Arctic Ocean
genre_facet Arctic Ocean
op_source Journal of Marine Science and Engineering, Vol 12, Iss 4, p 667 (2024)
op_relation https://www.mdpi.com/2077-1312/12/4/667
https://doaj.org/toc/2077-1312
doi:10.3390/jmse12040667
2077-1312
https://doaj.org/article/cfa7fa87cd9b47bfa21e2766301b963d
op_doi https://doi.org/10.3390/jmse12040667
container_title Journal of Marine Science and Engineering
container_volume 12
container_issue 4
container_start_page 667
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