Upper water column turbulence is often important to estuarine dynamics and constituent transport, yet our lack of comprehensive observations limits our understanding, and its prediction is a weakness of numerical models. Here, we describe observations of turbulence over a range of wind and tidal forcing in the Hudson River estuary and preliminary comparisons of the observations against a series of empirical and theoretical models of increasing complexity. A field experiment was conducted along a broad 5 m deep section of the Hudson over one month in fall, 2007. An autonomous instrumented catamaran was anchored near a bottom-mounted 1200 kHz acoustic Doppler current profiler that was measuring vertical profiles of velocity and several turbulence parameters using the variance method. The catamaran held an acoustic Doppler velocimeter, a sonic anemometer, an inertial sensor, and other instrumentation (e.g. carbon dioxide air-sea fluxes). Anchor stations (12-hour) and along- and across-channel transects were conducted from a small boat with CTD profiling to observe density stratification. Of particular interest are the effects of tidal currents and a superimposed along-estuary wind ......
CITATION STYLE
Orton, P. M., McGillis, W. R., & Zappa, C. J. (2008). Tide and wind forcing of estuarine upper water column turbulence. AGU . American Geophysical Union.
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