Characterization of Tidal Currents in Monterey Bay from Remote and In-Situ Measurements
NAVAL POSTGRADUATE SCHOOL MONTEREY CA
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A first order description of tidal heights and currents in Monterey Bay is provided. Analysis of sea level records indicate that a mixed, predominantly semidiurnal tide nearly co-oscillates within the bay. Analysis of month-long moored ADCP records obtained in the winter and summer of 1992 reveals that tidal-band currents account for approximately 50 percent of the total current variance in the upper ocean 20-200 m. A relatively strong 7 cms fortnightly tide MSf is present in both seasons. Considerable rotation of the semidiurnal ellipse orientations occurs with depth during both seasons. A month- long record of surface current measurements obtained with CODAR, an HF radar system, during September 1992 reveals that the Monterey Submarine Canyon clearly influences the strength and direction of semidiurnal M2 tidal currents. Good agreement exists between the strength and orientation of ADCP- and CODAR-derived tidal ellipses, with the exception of the constituent K1. Large, spatially uniform K1 surface currents 20-30 cms appear to be the result of diurnal sea breeze forcing.
- Physical and Dynamic Oceanography