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Climate Dynamics · 2025 · Vol. 63 · Issue 10 · Springer
Variation of sea surface temperature (SST) results from a host of mechanisms involving both the ocean and atmosphere. The atmospheric forcing on SST is usually hypothesized as white noise to reflect the transient and chaotic nature of the atmosphere in contrast to the large heat inertial of the ocean mixed layer. This study presents evidence that the non-white-noise memory of atmospheric forcing has a substantial contribution...