physics.geo-phJul 28, 2026

A Spatial Persistence Gradient in European Warming Consistent with North Atlantic Cold-Blob Influence

Authors: Mauricio Herrera-Marín, Alex Godoy-Faúndez, Diego Rivera

Organizations: Research Center on Sustainability and Strategic Resource Management (CISGER), Faculty of Engineering, Universidad del Desarrollo, Avda. Plaza 700, Santiago, Chile.

Abstract

Europe is warming faster than the global mean, yet the spatial organisation of this acceleration remains incompletely understood. Using ERA5 reanalysis for 1950--2024 across 28 IPCC AR6 European sub-regions, we identify two connected empirical results. First, the DFA1 Hurst exponent of interannual temperature residuals is strongly and negatively associated with the 1996--2024 warming rate (r=−0.792r=-0.792, p=5.1×10−7p=5.1\times10^{-7}). High-persistence, mainly Atlantic-proximal regions warm more slowly, whereas low-persistence continental regions warm faster. This relationship is robust to five residualisation schemes, three memory estimators, leave-one-region-out analysis, and five null-test families, including spatial block permutation. It also persists across warming windows (r=−0.550r=-0.550 for 1981--2024, −0.792-0.792 for 1996--2024, and −0.875-0.875 for 2000--2024), but vanishes under DFA2, indicating that the signal lies in low-frequency interannual-to-decadal persistence rather than trend curvature. The pattern is consistent with, but does not prove, North Atlantic cold-blob and thermohaline influence on European land temperatures. Second, under a strict 2006--2024 holdout, contemporaneous Mediterranean SST reduces mean annual temperature RMSE by 43% (from 0.7870.787 to 0.449,∘C0.449,^{\circ}\mathrm{C}). A causal lag-weight predictor based on prior-year Mediterranean and Atlantic SST also outperforms AR(2) (0.5780.578 versus 0.695,∘C0.695,^{\circ}\mathrm{C}) and remains informative after removing NAO, AO, and PNA effects. Similar skill from five-year moving-average and exponentially weighted predictors shows that short Mediterranean SST persistence at 1--5-year lags is the key predictive ingredient. Together, the results support a two-regime interpretation: Atlantic-proximal regions exhibit stronger memory and oceanic buffering, while continental interiors show faster warming and weaker interannual persistence.

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