ZedMikey
Well-Known Member
It apparently has to do with the stratification of water layers and nutrients for the phytoplankton. Cooler water has more nutrients and larger stratifications (which then allow deep water to bring even more nutrients to the surface).Any idea why that would be? On the surface (of the subject, not the ocean :flipoff:) it would seem that increased oceanic CO2 and temperature would cause plankton to grow more abundantly.
http://earthobservatory.nasa.gov/GlobalMaps/view.php?d1=MYD28M&d2=MY1DMM_CHLORA
Also from the paper in Nature...
Nature said:The effects of SST on Chl are probably explained by its influence on water column stability and MLD [mixed layer depth]. Increasing SST leads to a shallower mixed layer, which further limits nutrient supply to phytoplankton in already stratified tropical waters, but may benefit phytoplankton at higher latitudes where growth is constrained by light availability and deep mixing.
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