Changes in Arctic Halocline Waters Along the East Siberian Slope and in the Makarov Basin From 2007 to 2020
In the Arctic Ocean, the “halocline” is a cold near-surface layer where salinity increases rapidly with depth. The halocline isolates the sea ice at the surface from the heat stored in the underlying warm and salty water. Hence, the strength of the halocline is a key feature in the maintenance of th...
Main Authors: | , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2022
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Subjects: | |
Online Access: | https://zenodo.org/record/7083105 https://doi.org/10.5281/zenodo.7083105 |