A Tale of Two Estuaries: Columbia Bay, Alaska, and San Francisco Bay, California
Columbia Bay and San Francisco Bay are two estuaries that are opposites in almost every respect. Columbia Bay is a deep, high latitude fjord where dynamics are dominated by subglacial freshwater flows; San Francisco Bay is a shallow estuary dominated by tides and to a lesser extent by freshwater inflow. These different forcing mechanisms in conjunction with the dissimilar geometries, lead to different circulation patterns. These two particular estuaries provide examples of the wide range of circulation patterns found in estuaries.
KeywordsConvection Phytoplankton Stratification Posite Flushing
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- Cameron, W. M. and Pritchard, D. W. 1963 Estuaries. In The Sea, vol. 2. M. N. Hill, ed. Interscience, New York, pp 306–324.Google Scholar
- Cloern, J. E. 1979 Phytoplankton ecology of the San Francisco Bay System: The status of our current understanding. In San Francisco Bay: The urbanized estuary, pp. 247–264, T. J. Conomos, ed. Pacific Division of the American Association for the Advancement of Science, San Francisco.Google Scholar
- Conomos, T. J. 1979 Properties and circulation of the San Francisco Bay waters. In San Francisco Bay: The Urbanized Estuary, pp. 47–84, (Conomos, T. J., ed.), Pacific Division of the American Association for the Advancement of Science.Google Scholar
- Fischer, H. B. and Kirkland, W. B. 1978 Flushing of South San Francisco Bay. H. B. Fischer, Inc. Report HBF - 78/01.Google Scholar
- Meier, M. F. Rasmussen, L. A., and Miller, D. S. 1985 Columbia Glacier in 1984: disintegration underway. U.S. Geological Survey, Open-File Report 85–81, 17 PP.Google Scholar
- Muench, R. D. and Schmidt, G. M. 1975 Variations in the hydrographie structure of Prince William Sound. IMS Report R75–1. university of Alaska.Google Scholar
- Walters, R. A., Driedger, C. L. and Josberger, E. G. 1983 Subglacial discharge from Columbia Glacier (abs). EOS Transactions of the American Geophysical Union 64(45).Google Scholar