A Quasi-Dipole Structure in the Typical Summer Wind Forcing Over the California Current System Explains Spatial Variation in Coastal Water Temperature Anomalies During the Marine Heat Waves of 2014–2016
A Quasi-Dipole Structure in the Typical Summer Wind Forcing Over the California Current System Explains Spatial Variation in Coastal Water Temperature Anomalies During the Marine Heat Waves of 2014–2016