In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 122, No. 5 ( 2017-05), p. 3884-3906
Abstract:
Under winter storm winds, swift along‐shelf nearly‐barotropic flow was typically observed Flow fluctuations were primarily driven by variations of the sea‐surface gradient and not by local winds Under weak winds, a cross‐shelf density gradient developed that generated near‐surface currents of about 20 cm s −1
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1002/2016JC012102
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
detail.hit.zdb_id:
3094219-6
SSG:
16,13
