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P. (1978). Energy balance and wind effects in a shallow sound. J. Geophys. Res. 83, 4097-4106. Hicks, S. , and Crosby, J. E. (1974). Trends and variability of yearly mean sea level. NOAA Tech. Mem. NOS 13, 1-14. laniello, J. (1977). Nonlinearly induced residual currents in tidally dominated estuaries. D. Thesis, University of Connecticut, Storrs. Ippen. A. , and Harleman. D. R. F. Tidal dynamics of estuaries. In “Estuary and Coastline Hydrodynamics” (A. T. ), pp. 493-545. McGraw-Hill, New York.
To allow for this, we use an averaging period of 15 days in calculating the tidal energy flux. It is recognized that cross terms in (hv)due to lower frequency tidal constituents may not be negligible, but longer spans of data were not at hand. Simultaneous measurements of v and h were made at location J (Fig. 1) on the north-south section A-B through the middle of LIS. The measurements covered a 16-day period during which the winds were calm. The water depth was measured with a Bass model WG-100 wave gauge each hour and the current, with a General Oceanics model 20-10 current meter.
Meade, R. H. (1966). Salinity variations in the Connecticut River. Water Res. 2, 567-579. 38 ROBERT 9. GORDON Menard, H. W. (1961). Some rates of regional erosion. J. Geol. 69, 154-161. Morner, N. (1969). The late Quaternary history of the Kattegatt Sea and the Swedish west coast, deglaciation, shoreline displacement, chronology, isostasy and eustasy. , Sver. Geol. , Ser. C63, No. 3, 404-453. Newman, W. S. (1977). Late Quaternary paleoenvironmental reconstruction: Some considerations from northwestern Long Island, New York.