Seasonal variation of wind-driven diurnal current cycling on the Texas-Louisiana Continental Shelf

We describe observations of large amplitude wind-driven current oscillation s of 24-hr period occurring in the near-surface layer of waters of the Texa s-Louisiana continental shelf. The near-surface anti-cyclonic current ampli tudes can reach 60 cm s(-1) and represent the largest non-storm induced hig h-frequency currents on the shelf. These currents can persist for a week or more, as long as driving diurnal winds persist with uninterrupted phase. T he latitude of the shelf and the diurnal period of the wind-forcing combine to produce conditions for a near-resonant response of the surface currents to the wind stress, such that, the resulting currents are almost an order of magnitude greater than those found from steady Ekman drift. The oscillat ions are phase-locked to time of day suggesting a connection to the daily c ycle of heating and cooling. The oscillations generally occur during the su mmer months when there is a shallow mixed layer, strong vertical stratifica tion, maximum insolation, and infrequent frontal passages.