Estuarine Physics and Chemistry: Studies in Long Island by Barry Saltzman

By Barry Saltzman

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W. J. (1979). Seafloor stability in central Long Island Sound. Part I. Temporal changes in the erodibility of fine-grained sediment. In “Estuarine Interactions,” (M. L. ), pp. 221-244. Academic Press, New York. Schafer, J. P. (1979). The late Wisconsinan Laurentide ice sheet in New England. Geol. SOC. , Abstr. Programs 11, 52. Riley, G. A. (1956). Oceanography of Long Island Sound 1952-1954. 11. Physical oceanography. Bull. Bingham Oceanogr. Collect. 15, 15-46. Riley, G. A. (1967). Aspects of oceanography of Long Island Sound.

The average observed power is 53 MW. The decrease in energy STORM AND TIDAL ENERGY IN LONG ISLAND SOUND 45 10 1 N -0 w ou- h P %,' w 40- 20 0 ( 100 200 . - ~. 2. The total apparent tidal energy-crossing section A-B as calculated from h and v measured at J during calm weather. Curve L is the energy used in work done on the moon by the water within section A-B. after T = 270 hr in Fig. 2 is unexpected, since there is no obvious source from which power could flow seaward across section A-B for times longer than a semidiurnal tidal cycle.

41-87, State University of New York at Binghamton. Bowman, M. J. (1975). Pollution prediction model for Long Island Sound. Proc. , 3rd, 1975 pp. 1084-1103. Bowman, M. J. (1976a). Tidal locks across the East River: An engineering solution to the rehabilitation of Western Long Island Sound. I n “Estuarine Processes” (M. ), Vol. 1, pp. 28-43. Academic Press, New York. Bowman, M. J. (1976b). The tides of the East River, New York. J. Geophys. Res. 81, 1609- 1616. Bowman, M. , and Esaias, W. E. (1977).

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