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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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 |
_version_ |
1810430079204851712 |