Fig. 5
From: Future loss of Arctic sea-ice cover could drive a substantial decrease in California’s rainfall
Atmospheric impacts of Antarctic sea-ice loss. a Precipitation anomalies. b 500 hPa geopotential distribution changes. c Stream function changes. Shown are the ensemble mean differences (“low Arctic ice” minus control) for December–February (DJF) season. Stippling indicates anomalies that are statistically significant at the 90% confidence level
