Articles | Volume 11, issue 3
https://doi.org/10.5194/os-11-439-2015
https://doi.org/10.5194/os-11-439-2015
Research article
 | 
08 Jun 2015
Research article |  | 08 Jun 2015

Water level oscillations in Monterey Bay and Harbor

J. Park, W. V. Sweet, and R. Heitsenrether

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Cited articles

AMS: Seiches in Lake Garda, Mon. Weather Rev., 31, 532–533, https://doi.org/10.1175/1520-0493(1903)31[532b:SILG]2.0.CO;2, 1903.
AMS: The seiche and its mechanical explanation, Mon. Weather Rev., 34, 226, https://doi.org/10.1175/1520-0493(1906)34<226b:TSAIME>2.0.CO;2, 1906.
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Breaker, L. C., Broenkow, W. W., Watson, W. E., and Jo, Y.: Tidal and non-tidal oscillations in Elhorn Slough, California, Estuar. Coast., 31, 239–257, 2008.
Breaker, L. C., Tseng, Y., and Wang, X.: On the natural oscillations of Monterey Bay: observations, modeling, and origins, Prog. Oceanogr., 86, 380–395, https://doi.org/10.1016/j.pocean.2010.06.001, 2010.
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Short summary
Seiches in coastal bays can produce significant water level oscillations that impact maritime operations and introduce ecological stress. Monterey Bay, California, is found to have wave-driven short-period oscillations that can reinforce themselves, resulting in water level amplification. At longer periods the oscillations are not wave-driven and several potential forcing mechanisms are examined. A gyre offshore the bay is suggested as the driver, while other potential drivers are discounted.