In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 122, No. 8 ( 2017-08), p. 6611-6629
Abstract:
Glaciers grounded below the sill depth can renew fjord basins with subglacial discharge Wide fjords exhibit recirculation that increases dilution and residence time of glacially‐modified waters Tide‐sill interactions increase subglacial discharge‐driven transport of deep shelf waters into fjord basins
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1002/2017JC012962
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