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In: Mantoura RFC, Martin J-M and Wollast R (eds) Ocean Margin Processes in Global Change Dahlem . Meybeck M (1993) C, N, P and S in rivers: From sources to global inputs.

In: Mantoura RFC, Martin J-M and Wollast R (eds) Ocean Margin Processes in Global Change Dahlem Workshop Report. J Wiley & sons, Chichester pp 19–44Google Scholar. Brenon I, Le Hir P (1999) Modelling the Turbidity Maximum in the Scine Estuary (France): Identification of Formation Processes. Est Coast Shelf Sci 49:525–544CrossRefGoogle Scholar. In: Wollast R, Mackenzie FT, Chou L (eds) Interactions of C, N, P and S Biogeochemical Cycles and Global Change. NATO ASI Series, Vol. 14. Springer, Berlin pp 163–193CrossRefGoogle Scholar.

by Mantoura R F C and R. F. C. Mantoura.

1990, March 18-23 .

Ocean margin processes in global change : report of the Dahlem Workshop on Ocean Margin Processes in Global Change, Berlin, 1990, March 18-23 . Ocean margin processes in global change : report of the Dahlem Workshop on Ocean Margin Processes in Global Change, Berlin, 1990, March 18-23 .

Continental margin exchanges, in Ocean Biogeochemistry: A JGOFS Synthesis. and Wollast R. (eds). eds. Fasham, . Field, . Platt, T. and Zeitzschel,B. Kremer H. and Corssland . Ocean Margin Processes in Global Change. John Wiley and Sons, Chichester, 469 p. .

Dahlem Workshop on Ocean Margin Processes in Global Change (1990 : Berlin Freie Universität Berlin (author) T. D. Jickells R. Mantoura J. M. Martin Marga and Kurt Mollgaard Stiftung (author) R. Wollast (Ed. data.

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Two trends evident in global tidal modelling since the first GEOP conference in 1972 are described.

On behalf of the GEOP Steering Committee the conference was opened by Hyman Orlin (National Oceanic and Atmospheric nal Ocean Survey), program chairman, who, in his introductory. Two trends evident in global tidal modelling since the first GEOP conference in 1972 are described. The first centers on the incorporation of terms for ocean loading and gravitational self attraction into Laplace's tidal equations.