An empirical orthogonal function analysis of remotely sensed sea surface temperature variability and its relation to interior oceanic processes off Baja California

Abstract Empirical orthogonal function (EOF) analysis was applied to a 4.6-year sequence of AVHRR images off Baja California centered near Punta Eugenia to examine large-and mesoscale processes in this region of the California Current System (CCS). The mean structure found in the image sequence describes the seasonal cycle in sea surface temperature (SST) and the large-scale, north-south, oceanic SST gradient of the region. The first EOF-amplitude pair also describes the seasonal cycle in SST. Both results are consistent with long-term, large-scale, mean shipboard data for the region. The second EOF-amplitude pair defines two distinct regions paralleling the coast. The inshore region coincides with the coastal zone of Lynn and Simpson (1987), and the adjacent region farther offshore is identical to their transition zone . The third through fifth EOF-amplitude pairs primarily represent meandering of the California Current and anticyclonic mesoscale eddy occurrences in the region; these results also are consonant with a large number of shipboard observations. The EOF results provide independent satellite-derived evidence for the existence of a transition zone off Baja California which is similar to that found off central and southern California. Moreover, the agreement between the satellite-based results and the shipboard observations indicates that satellite data can be used successfully to study other current systems (e.g., Peru Current), where in situ observations (ships, buoys) are less abundant.

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