摘要
Long time series (18-64 years) of surface water temperature from 10 U.S. west coast shore stations from Oceanside in southern California to Neah Bay in Washington, were analyzed to evaluate the generality of results of the Scripps Institution regarding the predictability of internal tidal bores. Nine stations showed that temperature anomalies are predictable on average within the lunar cycle in spring or summer, but not in fall and winter. There is high variability in the magnitude and variance of the average anomaly among stations.