In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 128, No. 7 ( 2023-07)
Kurzfassung:
Interannual variability of the subsurface temperature maximum at Maud Rise is documented with observations Advection of anomalously cold and fresh deep waters from the Weddell Gyre into the Halo leads to a near‐vanishing of the Taylor Cap in 2014 Observed warming of the subsurface layer in the Taylor Cap due to eddy transport preceded the polynya opening in 2016–2017
Materialart:
Online-Ressource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2022JC019517
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2023
ZDB Id:
2016804-4
ZDB Id:
161667-5
ZDB Id:
3094219-6
SSG:
16,13