In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 122, No. 12 ( 2017-12), p. 9548-9571
Abstract:
Winter Weddell Sea pack ice (Antarctica) remains warm and permeable due to large snow depth and frequent occurrence of warm cyclonic events These conditions trigger brine dynamics and associated sea ice biogeochemical processes Of the limited number of winter Weddell Sea pack ice studies (3), this one reveals higher snow depth, negative freeboard, and higher Chl‐ a
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1002/jgrc.v122.12
DOI:
10.1002/2017JC013288
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