In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 129, No. 3 ( 2024-03)
Abstract:
The simulated hydrographic structures over the Bellingshausen Sea continental shelf region are in good agreement with observations The warm water intrusions toward the Venable Ice Shelf show peaks of higher velocities in summer, likely caused by coastal trapped waves Glacial meltwater from about 33% of the area underneath the BS ice shelves flows into the Amundsen Sea within 2 years
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2022JC019275
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2024
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
detail.hit.zdb_id:
3094219-6
SSG:
16,13
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