Abstract

Details of the annual thermocline cycle in the coastal area off San Diego have been determined from temperature data recorded hourly for over a year at the Naval Undersea Research and Development Center Oceanographic Tower. Vertical thermal gradients averaged 0.59°C/m at their strongest part from late April through early September. The sharpest gradients, which occurred in late June, were as great as 1.27°C/m. Transient gradients averaging 0.29°C/m at their strongest part occurred frequently in late March and early April and from late September through early November. Weak thermal gradients averaging 0.15°C/m at their sharpest predominated from late November through early March. Water temperature varied from 9.7° to 23.6°C. Internal tides persisted throughout the year, contributing to monthly temperature variances that ranged from 0.2 (°C)2 in January to 5.6 (°C)2 in May and August.

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