In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 48, No. 9 ( 2021-05-16)
Abstract:
The North American proglacial lakes induce an ice sheet instability during the last deglaciation This instability is mechanically driven even though it is triggered by surface mass balance The instability could explain half of the mass loss when the ice sheet reaches the region of the present‐day Hudson Bay
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2020GL092141
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13