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The turbulent air-sea heat flux feedback ( $$\alpha$$ α , in $$\text {W m}^{-2}\text { K}^{-1}$$ W m - 2 K - 1 ) is a major contributor to setting the damping timescale of sea surface temperature (SST) anomalies. In this study we compare the spatial distribution and magnitude of $$\alpha$$ α in the North Atlantic and the Southern Ocean, as estimated from the ERA-Interim...
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