Wintertime Cross-correlational Structures between Sea Surface Temperature Anomaly and Atmospheric-and-Oceanic Fields in the East/Japan Sea Under Arctic Oscillation

The winter Arctic Oscillation (AO) modulates East Asian climate and the East/Japan Sea (EJS), yet local, scale-dependent air-sea couplings linking atmosphere, ocean and sea-surface temperature anomalies (SSTA) remain unclear. Using 30 years of daily fields (1993–2022), we compute detrended fluctuation/cross-correlation metrics over 5–50-day scales at every grid: the Hurst exponent ($H$), the cross-Hurst exponent ($\lambda$), and the DCCA coefficient (${\rho }_{DCCA}$). Significance is assessed with iterative-AAFT surrogates and Benjamini–Hochberg false-discovery-rate control. Three robust features emerge. (1) During AO+ winters, the EKB–SPF corridor exhibits high SSTA variance and near-ballistic persistence ($H\approx 1.4$–$1.5$), indicating increased susceptibility to marine heatwaves. (2) SSTA co-fluctuates positively with near-surface air-temperature anomalies, whereas turbulent heat-flux anomalies are largely anti-phased and show negligible cross-persistence, consistent with fast damping. (3) Oceanic fields impart persistent coupling: sea-surface height anomalies display basin-wide positive links with SSTA; meridional geostrophic velocity imprints advective cross-coupling along EKWC/SPF pathways, while zonal flow and vorticity yield patchy signatures. Winter SST variability in the EJS thus reflects a two-tier process in which mesoscale structure and along-front advection organize persistence, while synoptic forcing and turbulent heat exchange supply strong but non-persistent tendencies. The FDR-controlled, grid-point DFA/DCCA framework is transferable to other marginal seas.