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Daniel Swain
weatherwest.bsky.social
did:plc:gslrbg7et2wxhlhrkqtwlm22
This is a classic "warm West/cool East" pattern, representing an amplification of winter mean state stationary wave pattern (which consists of a Western ridge and Eastern trough). It often yields a dramatic temperature contrast across continental U.S. https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2016JD025116
2026-01-19T23:00:51.733Z