Tidal and Long-term Flow Through Two Tidal Channels Connecting Southern Biscayne Bay and Card Sound With Atlantic Shelf Waters
Current meter data and local wind measurements from a 166-d study in 1996–97 are used to describe tidal and long-term flow through two tidal channels that connect southern Biscayne Bay and Card Sound with Atlantic shelf waters. Results indicate a quasisteady, long-term outflow from the estuary through Caesar Creek and Angelfish Creek that averaged 12 cm s−1 and 8 cm s−1, respectively. Harmonic analysis indicates that the tides dominate the instantaneous flow through the channels, with diurnal and semi-diur- nal tidal constituents accounting for 85–87% of the total variance. M2 amplitudes for Caesar Creek and Angelfish Creek are 72 and 52 cm s−1, respectively. Comparisons of local winds and along-channel currents indicate that wind stress plays the primary role in driving the nontidal flow through the channels. Spectral analysis shows high coherence between along-channel currents and a broad range of wind stress components over time scales of 2–16 d. Winds from the northern sector show particularly high coherence with along-channel flow through both creeks, accounting for 40–80% of the variance in nontidal along-channel flow over the low-frequency time scales. A close inspection of the seasonal and low-frequency wind stress pattern, however, suggests that the long-term outflow observed through the two channels is not due to wind stress alone. A comparison of freshwater flux in the bay with channel outflow indicated a marginal cause-and-effect relationship. Surface runoff and precipitation explain only 2–3% of the variance in outflow through the two channels.
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Document Type: Research Article
Publication date: 2000-11-01
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