Abstract:1) Atmospheric oxygen cycles on a seasonal basis, as does carbon dioxide.
2) Photosynthesis is likely contributing to these cycles, but the dominant spatial regions are unknown and the contribution of marine plankton has been assumed to be small.
3) I test and confirm the prediction that seasonal sea ice and oxygen rates are highly coherent at high latitudes, with peak oxygen emission in months of peak rates of sea ice loss within each Hemisphere.
4) The similarity of oxygen dynamics in Northern and Sout… Show more
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