In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 36, No. 10 ( 2022-10)
Abstract:
A new, dynamic marine particle cycling model reproduces the observed attenuation of sinking particulate organic carbon fluxes at 22 locations Particle properties, ocean temperature, and to a lesser extent, seawater viscosity explain most of the large‐scale differences in mesopelagic carbon transfer efficiency Particles transport organic carbon downward more efficiently at high latitudes than at low latitudes, consistent with recent studies
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2021GB007131
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2022
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13