Ocean and Cryosphere in a Changing Local weather.
The transport enhance outcomes from stronger northward flows (not fewer southward stream events), yielding a one hundred fifty% enhance in kinetic power, presumably with impacts on bottom suspension, mixing, and erosion. Based on their research, the authors imagine that the traditional framework for the subpolar Southern Ocean carbon cycle essentially misrepresents the drivers of regional carbon uptake. The article discusses the Atlantification” and Pacification” of the Arctic Ocean as warming waters permitting new species to migrate northward and
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