. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Two-dimensional circulation model 319 distance over which 5^o-i5%0 at the bottom of the estuary, is a strong function of fresh- water discharge. It increases from 44 km for Uf = 4 cm/s to 170 km for U( = 0-5 cm/s as shown in Figures 5 and 6. This behavior has been empirically, if qualitatively, known to hydraulic engineers for many years. The functional form of the dependence of salinity intrusion upon freshwater discharge is of special interest bec
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Two-dimensional circulation model 319 distance over which 5^o-i5%0 at the bottom of the estuary, is a strong function of fresh- water discharge. It increases from 44 km for Uf = 4 cm/s to 170 km for U( = 0-5 cm/s as shown in Figures 5 and 6. This behavior has been empirically, if qualitatively, known to hydraulic engineers for many years. The functional form of the dependence of salinity intrusion upon freshwater discharge is of special interest because a characteristic value of Uf in coastal plain estuaries is approximately 1 cm/s. It is apparent from Figure 6 that for the values of other parameters used, the length of salinity intrusion changes behavior in the. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Atlantic Oceanographic and Meteorological Laboratories; Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories; Environmental Research Laboratories (U. S. ). Washington, D. C. : U. S. Dept. of Commerce, Environmental Science Services Administration, Research Laboratories : For sale by Supt. of Docs. U. S. G. P. O.
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