In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 127, No. 8 ( 2022-08)
Abstract:
The heat loss from the Atlantic Water inflow North of Svalbard varies between 302 W m −2 in winter and 60 W m −2 in spring A surface countercurrent on the upper slope carrying transformed Atlantic Water is modulated by the Atlantic Water inflow and Ekman setup An offshore bottom‐intensified current is detected on the lower slope, partly correlated with the wind stress curl
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2022JC018568
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2022
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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