By Gould R.F. (ed.)
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A carefulconsideration of theseaspects should,therefore,precede anybiologicaL/oceanographical investigation. The followingreviewof the hydrography of the DanishStraitsin relationto eutrophication will in more detailillustrate thislink between theassessment of thebiologicalproblemandthe hydrographic analysis. ) (1) wheret is time,x is theCartesian coordinate, u is the mean(nonturbulent) flow velocity, c istheconcentration of matter,u' andc' aretheturbulentpartof u and Moller 55 andT is a termexpressing theinteraction between compartments.
The North Seaand the Black Seaillustratethe importanceof the hydrographic conditions for thedevelopment of eutrophication effects. Alsothe 54 3. Water Masses,Stratificationand Circulation processes of theDanishStraitsandcoastal watersarestronglyinfluenced by thehydrography. In thefollowing, thebasicphysical phenomena of theDanishStraitsare described, andit is seenthatmanyof thehydrographic processes identifiedin the BlackSeaandNorth Seaalsoprevailin thesecoastalareas. Generally,however, it is not possibleto solvethe equationsand expressthe transportand mixing of matterin the oceanwithoutintroducingsimplifyingassumptions.
R. ,17, 347-352, 1983. ,andD. R. Schreiber, Useof theionpairingmodelto estimate activitycoefficientsof naturalwaters,Am. J. ,282, 1508-1540, 1982. , andG. Schumann, Mechanisms of transport fromtheatmosphere to theearth's surface, J. Geophys. ,75, 3013-3019, 1970. ,27A,261-270,1993. ,andR. M. ,26A, 16891699, 1992. Pacyna, J. , S. Larssen, andA. ,25A, 425-439, 1991. Paerl,H. , andM. L. Fogel,Isotopiccharacterization of atmospheric nitrogeninputsas sources of enhanced primaryproduction in coastalAtlanticOceanwaters,Mar.