Over 30 winters, persistent warmth in the East/Japan Sea lines up with sea-surface height and along-front currents, while winds and heat fluxes act only as short-lived, non-persistent forcing.
Impact of Arctic Oscillation on the East Asian climate: A review
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Wintertime Cross-correlational Structures between Sea Surface Temperature Anomaly and Atmospheric-and-Oceanic Fields in the East/Japan Sea Under Arctic Oscillation
Over 30 winters, persistent warmth in the East/Japan Sea lines up with sea-surface height and along-front currents, while winds and heat fluxes act only as short-lived, non-persistent forcing.