Changes in ocean circulation and carbon storage are decoupled from air-sea CO<sub>2</sub> fluxes
The spatial distribution of the air-sea flux of carbon dioxide is a poor indicator of the underlying ocean circulation and of ocean carbon storage. The weak dependence on circulation arises because mixing-driven changes in solubility-driven and biologically-driven air-sea fluxes largely cancel out....
Main Authors: | A. Gnanadesikan, I. Marinov |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2011-02-01
|
Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/8/505/2011/bg-8-505-2011.pdf |
Similar Items
-
Sea–air CO<sub>2</sub> fluxes in the Indian Ocean between 1990 and 2009
by: V. V. S. S. Sarma, et al.
Published: (2013-11-01) -
Air–sea CO<sub>2</sub> flux in the Pacific Ocean for the period 1990–2009
by: M. Ishii, et al.
Published: (2014-02-01) -
Sea–air CO<sub>2</sub> fluxes in the Southern Ocean for the period 1990–2009
by: A. Lenton, et al.
Published: (2013-06-01) -
Air-sea CO<sub>2</sub> fluxes on the Bering Sea shelf
by: M. A. Jeffries, et al.
Published: (2011-05-01) -
Interannual variability of air-sea CO<sub>2</sub> fluxes and carbon system in the East Siberian Sea
by: I. Wåhlström, et al.
Published: (2011-07-01)