Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015
We examined vertical profiles of methane (CH4) concentrations inside and outside of a warm-core eddy during a cruise of the R/V Mirai cruise (MR15-03 Leg. 1) in the Arctic Ocean in late summer/early fall 2015. Because a coherent mesoscale eddy is one of the possible mechanisms for transporting shelf...
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Format: | Article in Journal/Newspaper |
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Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15998 http://id.nii.ac.jp/1291/00015888/ |
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ftnipr:oai:nipr.repo.nii.ac.jp:00015998 2023-05-15T14:57:48+02:00 Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 2019-12 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15998 http://id.nii.ac.jp/1291/00015888/ en eng https://doi.org/10.1016/j.polar.2019.100481 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15998 http://id.nii.ac.jp/1291/00015888/ Polar Science, 22, 100481(2019-12) 18739652 Arctic ocean Dissolved methane Warm-core eddy Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2019.100481 2022-12-03T19:43:16Z We examined vertical profiles of methane (CH4) concentrations inside and outside of a warm-core eddy during a cruise of the R/V Mirai cruise (MR15-03 Leg. 1) in the Arctic Ocean in late summer/early fall 2015. Because a coherent mesoscale eddy is one of the possible mechanisms for transporting shelf water from the Chukchi Sea into the Canada Basin interior, we hypothesized that the warm-core eddy transported dissolved CH4 as well as nutrients and impacted the distribution of CH4. Seawater samples were therefore collected to obtain detailed vertical profiles of CH4 concentrations in the southwestern Canada Basin. We found high CH4 concentrations in bottom water on the shelf, which was located outside the warm-core eddy. The percent saturation in that water was as high as 947% of atmospheric CH4. We also found that sub-surface CH4 peaks within the radius of the maximum velocity of the eddy were broader at depth than those outside of the eddy. Lateral transport of the eddy was likely the controlling factor responsible for subsurface CH4 peaks within the warm-core eddy. Our study indicated that eddies play a crucial role in controlling and transporting CH4 laterally and vertically. Article in Journal/Newspaper Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Polar Science Polar Science National Institute of Polar Research Repository, Japan Arctic Arctic Ocean Chukchi Sea Canada Polar Science 22 100481 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Arctic ocean Dissolved methane Warm-core eddy |
spellingShingle |
Arctic ocean Dissolved methane Warm-core eddy Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
topic_facet |
Arctic ocean Dissolved methane Warm-core eddy |
description |
We examined vertical profiles of methane (CH4) concentrations inside and outside of a warm-core eddy during a cruise of the R/V Mirai cruise (MR15-03 Leg. 1) in the Arctic Ocean in late summer/early fall 2015. Because a coherent mesoscale eddy is one of the possible mechanisms for transporting shelf water from the Chukchi Sea into the Canada Basin interior, we hypothesized that the warm-core eddy transported dissolved CH4 as well as nutrients and impacted the distribution of CH4. Seawater samples were therefore collected to obtain detailed vertical profiles of CH4 concentrations in the southwestern Canada Basin. We found high CH4 concentrations in bottom water on the shelf, which was located outside the warm-core eddy. The percent saturation in that water was as high as 947% of atmospheric CH4. We also found that sub-surface CH4 peaks within the radius of the maximum velocity of the eddy were broader at depth than those outside of the eddy. Lateral transport of the eddy was likely the controlling factor responsible for subsurface CH4 peaks within the warm-core eddy. Our study indicated that eddies play a crucial role in controlling and transporting CH4 laterally and vertically. |
format |
Article in Journal/Newspaper |
title |
Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
title_short |
Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
title_full |
Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
title_fullStr |
Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
title_full_unstemmed |
Influence of warm-core eddy on dissolved methane distributions in the southwestern Canada basin during late summer/early fall 2015 |
title_sort |
influence of warm-core eddy on dissolved methane distributions in the southwestern canada basin during late summer/early fall 2015 |
publishDate |
2019 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15998 http://id.nii.ac.jp/1291/00015888/ |
geographic |
Arctic Arctic Ocean Chukchi Sea Canada |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea Canada |
genre |
Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Polar Science Polar Science |
genre_facet |
Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Polar Science Polar Science |
op_relation |
https://doi.org/10.1016/j.polar.2019.100481 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15998 http://id.nii.ac.jp/1291/00015888/ Polar Science, 22, 100481(2019-12) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2019.100481 |
container_title |
Polar Science |
container_volume |
22 |
container_start_page |
100481 |
_version_ |
1766329916672966656 |