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By Eremeev

This ebook includes articles via oceanographic researchers from the (former) USSR and provides new facts on a number of facets of the Black Sea. the themes contain Black Sea thermohaline, hydrochemical and optical buildings, the dynamics of the most Black Sea present and deep layers, wave phenomena in shelf components and modelling of advanced marine platforms. Aslo integrated are a few experimentally derived effects which enable a Read more...

summary: This publication includes articles by means of oceanographic researchers from the (former) USSR and offers new facts on a number of facets of the Black Sea. the subjects comprise Black Sea thermohaline, hydrochemical and optical buildings, the dynamics of the most Black Sea present and deep layers, wave phenomena in shelf parts and modelling of complicated marine structures. Aslo incorporated are a few experimentally derived effects which permit a deeper perception into the matter of O2 and H2S coexistence within the Black Sea. The standard notions concerning the constitution of the oxic/anoxic interface are seriously evaluated

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For profile 1 (Fig. 058 and shelf width is 5 km; for profile 3 (Fig. 025 and 46 km, respectively. 4 h (A = 116 km), respectively (Fig. l a ) . As is readily visualized, phase velocity of the profile 3 shelf wave is considerably larger than this in the case of profile 1. 5 h. The role of geometry of the continental slope here is relatively modest: profiles 2 and 4 (Fig. l a ) have similar values of shelf width and wavelength. 016, respectively. 4 h, the wavelengths being 58 and 79 km, respectively.

Kikhai, Yu. V. Preliminary digital processing of the side-looking radar images. Moscow: Tr. 2-go Vsesoyuzn. soveshch. po sputnic. gidrofizike (Sevastopol, 8-12 October, 1985), (1986), Dep. VINITI, 67-72. 9. Ivanchik, M. V. and Krovotyntsev, V. A. Analytical method for rough geodesical downlinking of meteorological satellite-provided scanner images using reference points. Issled. Zemli iz Kosmosa (1987), 109-115. phic Research of the Black Sea, pp. 5 1 - 5 9 © VSP 1992. Some peculiarities of the sea surface dynamics in the deep section of the Black Sea A.

5xl05m, 3 #0=2xl0 m, 61 = 1 . 2 x l 0 5 m , mi = 18, m 2 = 10, &2 = l . 37 x 10 m. 5, and 5. Approximately similar values are characteristic of the Black Sea coastal area during winter, spring, and summer time. The value of £ in autumn is close to that observed in spring time. In addition, the atmospheric pressure amplitude will be assumed constant (/(y) = 1) or varying by the law / ( y ) = cos #i and S\ = try/2b. 2) simulate geometry of the bottom features and of the undisturbed surface of the density gradient between the Crimea and the Anatolian coast (see Fig.

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