By Dr. Victor S. Kennedy
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Additional info for Estuarine Comparisons. Proceedings of the Sixth Biennial International Estuarine Research Conference, Gleneden Beach, Oregon, November 1–6, 1981
Much of this variability was due to internal waves. 5 m and they have been interpreted as due to lateral inter nal seiching (Dyer 1982). However, there are many broader features that persist from one tide to another, undergoing progressive modification. Salinity %o y 2400 1 1 1 1 1 0200 0400 0600 0800 1000 1 1000 1 1400 1200 1400 1 1200 1600 ^ 1600 2000 1800 2000 1——I 1800 2200 r 2200 \ \ 2400 1 2400 1 \ \ Γ 1 1 ^—^ ^ - Figure 31A}. Time sequence oj salinity and velocity variation at Station 1.
Circulation and salinity distribution in coastal Louisiana estuaries. Contr. Mar. Sei. 20:1-10. Kjerfve, B. 1978. Bathymetry as an indicator of net circulation in well-mixed estuaries. Limnol. Oceanogr. 23:816-821. Kjerfve, B. and H . N . McKellar, Jr. 1980. Time series measurements of estuarine material fluxes, pp. 341-357. In: V. S. ), Estuarine Perspectives. Academic Press, New York. Kjerfve, B. and J. A . Proehl. 1979. Velocity variability in a cross-section of a well-mixed estuary. J. Mar.
5 h for eight tidal cycles during four seasons. The present study was a preliminary calibration study to aid in the design of Outwelling. The field experiment in March 1978 in South Jones Creek was con ducted to test whether the sampling design and analysis techniques would yield flow continuity. 5 h for two tidal cycles at sections B, C, and D, w e hoped that the data would indicate that equal amounts of water moved through Β, Kjerfve et al. 50 SOUTH JONES MARCH 11 1978 CREEK 04 0« MARCH 12 Figure 8.