In:
Journal of Geophysical Research: Earth Surface, American Geophysical Union (AGU), Vol. 124, No. 4 ( 2019-04), p. 920-937
Abstract:
The thawing of ice‐bearing subsea permafrost was modeled by coupling heat and salt diffusion The boundary conditions reflect sea ice dynamics during the transition from terrestrial to marine permafrost The modeled ice‐bearing permafrost depths were validated with geoelectric surveys
Type of Medium:
Online Resource
ISSN:
2169-9003
,
2169-9011
DOI:
10.1029/2018JF004823
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2130824-X
detail.hit.zdb_id:
2138320-0
SSG:
16,13