In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 123, No. 11 ( 2018-11), p. 8203-8226
Abstract:
The Cold Pool travels equatorward along the 60‐m isobath at a speed of 2–3 cm/s with a warming rate of about one degree Celsius per month The northern extent of the Cold Pool retreats 2.6 times faster than the southern extent Vertical and horizontal advection, rather than vertical diffusion, modulate the geographical differences in warming trends
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2018JC014148
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
detail.hit.zdb_id:
3094219-6
SSG:
16,13