A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA
Under coastal fast ice in the Ongul Strait near Syowa Station, Antarctica, warmer, more saline, and oxygen-poorer water appears in mid-depth and deep layers from winter to spring every year. This water is explained as a result of mixing between Circumpolar Deep Water (CDW) and Winter Water (WW). Thi...
Main Authors: | , , , |
---|---|
Format: | Report |
Language: | English |
Published: |
Institute of Low Temperature Science, Hokkaido University
1991
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3644 http://id.nii.ac.jp/1291/00003644/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3644&item_no=1&attribute_id=18&file_no=1 |