In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 129, No. 3 ( 2024-03)
Abstract:
Mesoscale‐resolving ocean biogeochemistry simulations show vertical mixing is a key source of oxygen to the equatorial Pacific thermocline The supply of oxygen by advection and vertical mixing is strongly seasonal and is driven by seasonal variability in the wind The vertical mixing of oxygen is modulated by the wind stress and mesoscale eddy impacts on equatorial shear‐driven turbulence
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2023JC020588
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2024
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
detail.hit.zdb_id:
3094219-6
SSG:
16,13