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- W1972502612 abstract "Significant warming has occurred across many ocean basins over the past 50-years. This has been observed through an increase in the oceanic heat content (OHC) which describes the depth integrated temperature change. The OHC trend displays a maximum value (ie. warming) in the midlatitude band stretching from 35°–50°S. However, this warming pattern is unable to be accounted for by changes in local heat fluxes. It is associated with a Sverdrup-like response to poleward strengthening winds and a poleward shift of the Southern Hemisphere supergyre and Antarctic Circumpolar Current of almost 1°. The heat required for this midlatitude warming is mostly derived from surface heat fluxes from south of 50°S, which is advected northward by enhanced Ekman transport induced by the poleward-strengthening winds. These results highlight the relationship between winds and surface heat fluxes in Southern Hemisphere midlatitude oceans." @default.
- W1972502612 created "2016-06-24" @default.
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- W1972502612 date "2010-05-01" @default.
- W1972502612 modified "2023-09-25" @default.
- W1972502612 title "What is driving the fast warming rate of the Southern Hemisphere midlatitude ocean?" @default.
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- W1972502612 doi "https://doi.org/10.1109/oceanssyd.2010.5603876" @default.
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