Model output from the suite with differing isopycnal mixing coefficients reported in
Pradal, Marie-Aude and Anand Gnanadesikan, 2014: How does the Redi parameter for mesoscale mixing impact global climate in an Earth System Model?, Journal of Advances in Modeling the Earth System, 6,586-601,doi:10.1002/2013MS000273, Link
Gnanadesikan, Anand, Marie-Aude Pradal and Ryan Abernathey, 2015: Isopycnal mixing by mesoscale eddies significantly impacts oceanic anthropogenic carbon uptake, Geophys. Res. Lett.. 42,4249-4255, doi:10.1002/2015GL064100 [Link]
Gnanadesikan, Anand, Marie-Aude Pradal and Ryan Abernathey, Changes in the isopycnal mixing coefficient produce significant, but compensated, changes in ocean carbon pumps,subm. Global Biogeochemical Cycles. [Link]
Datasets here are
ARedi=400 m2/s: Download [Ocean physics], [BLING biogeochemistry]
ARedi=800 m2/s: Download [Ocean physics], [BLING biogeochemistry] [ Atmosphere ]
ARedi=1200 m2/s: Download [Ocean physics], [BLING biogeochemistry]
ARedi=2400 m2/s: Download [Ocean physics], [BLING biogeochemistry]
Aredi=Abernathey and Marshall (2013): Download [Ocean physics], [BLING biogeochemistry]
Aredi=Zonally averaged Abernathey and Marshall (2013): Download [Ocean physics], [BLING biogeochemistry]
Modern Black carbon run: [ Atmosphere ]