Fig. 3: Arctic SIC anomalies linked to SCEII variations.
From: A dynamic link between spring Arctic sea ice and the Tibetan Plateau snow increment indicator
Spatial distribution of lagged correlation coefficients between SCEII and Arctic SIC during 1979–2021 in a OND, b DJF and c FMA. Information flow (unit: nats) from SCEII to Arctic SIC in d OND, e DJF and f FMA. The stippled regions denote the statistical significance at the 5% level.
