Co-variability of Pacific‐Atlantic SST contrast, Caribbean Sea tropical rainfall and U.S. summer to fall rainfall variability

In the U.S., peak summer (June-July) rainfall variability, especially east of the Rockies, is largely linked to North Atlantic sea surface temperature (SST) anomalies and associated variations in the Bermuda High. However, these well-established relationships almost completely break down in late summer to mid fall (August-October). Thus, operational seasonal forecast models have generally low skill... Continue Reading →

Powered by WordPress.com.

Up ↑