Complex Oceanographic Research on the Black Sea by Eremeev

By Eremeev

This booklet includes articles through oceanographic researchers from the (former) USSR and offers new facts on quite a few elements of the Black Sea. the themes contain Black Sea thermohaline, hydrochemical and optical constructions, the dynamics of the most Black Sea present and deep layers, wave phenomena in shelf components and modelling of complicated marine platforms. Aslo incorporated are a few experimentally derived effects which permit a Read more...

summary: This publication includes articles by means of oceanographic researchers from the (former) USSR and provides new info on a variety 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 advanced marine platforms. Aslo incorporated are a few experimentally derived effects which enable a deeper perception into the matter of O2 and H2S coexistence within the Black Sea. The normal notions in regards to the constitution of the oxic/anoxic interface are seriously evaluated

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5 m s - 1 , and in the central Some peculiarities of the sea surface dynamics 53 Figure 1. The pattern of surface water circulation in October 1985 (small arrows are current vectors). 5 m s" 1 . 45 m s " 1 (Fig. 2b). 37 m s " 1 . 13 m s - 1 velocities oriented southwestward were observed: these obviously take their origin inside the western cyclonic gyre at its western boundary.

L a ) h* = 125 m and for profile 3 V. A. Ivanov and A. E. Yankovsky 28 (Fig. l a ) ft* = 180 m; the shelf break for both profiles corresponds to the 100 m isobath (Fig. l a ) . However, in the case of profile 1, shelf width is merely 5 km, whilst in the case of profile 3, it equals 46 km. Owing to this, edge waves corresponding to profile 3 have larger space-time scales: period T is equal to 1 h 58 min to 2 h 6 min and the wavelength ranges from 300 to 395 km (Fig. 2). For profile 1, these quantities are equal to 11-15 min and 25-45 km, respectively (Table 1).

4. Hasse, J. On the surface to geostrophic wind relationship at sea and stability dependence of the resistance law. Phys. Atmos. (1974), 45 p. 5. V. On the analysis and reconstruction of meteorological fields using the method of statistical testing. Works of the USSR Hydrometeorological Center (1976), 83-88. 6. , Bossr, D. , et al. The relationship between wind vector and normalized radar cross section used to derive SEASAT-A satellite scatterometer winds. J. Geophys. Res. (1982 ) 87, 3318-3336.

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