Sea-ice motion and oceanographic data from the Beaufort Sea to the Chukchi Borderland in March–December 2020
Sea-ice reduction is one of the most visible indicators of the Arctic warming. While thereare many observations in the interior of the Arctic Ocean, oceanographic and sea-ice trajectory observations near the edge of sea-ice extent are rare. Here, we present oceanographic observations beneath sea ice...
| Format: | Article in Journal/Newspaper |
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| Language: | English |
| Published: |
National Institute of Polar Research
2021
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| Online Access: | http://id.nii.ac.jp/1434/00000027/ https://pdr.repo.nii.ac.jp/?action=repository_uri&item_id=41 https://pdr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=41&item_no=1&attribute_id=22&file_no=1 https://pdr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=41&item_no=1&attribute_id=22&file_no=2 https://pdr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=41&item_no=1&attribute_id=22&file_no=3 |
| Summary: | Sea-ice reduction is one of the most visible indicators of the Arctic warming. While thereare many observations in the interior of the Arctic Ocean, oceanographic and sea-ice trajectory observations near the edge of sea-ice extent are rare. Here, we present oceanographic observations beneath sea ice obtained by an ice-tethered buoy and surrounding sea-ice motions obtained from 9 GPS buoys in the late ice-growth and sea-ice melt season along trajectories from the Beaufort Sea to the Chukchi Borderland in the Pacific sector of the Arctic Ocean. |
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