Computational algorithm for the evaluation of inclinations of the level in the problems of the dynamics of basins

We develop a method for the evaluation of inclinations of the level, which enables one to find them with high accuracy. The reliability of this method is tested by comparing the numerical solutions for inclinations of the level with analytic expressions. It is shown that the system of coupled equations for inclinations of the level can be decomposed into two independent equations with sufficiently high accuracy. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Diffusion in the ocean with diffusion coefficient depending on the scale and concentration of impurities

We solve a nonlinear problem of diffusion from a concentrated source in a moving medium with diffusion coefficient depending on the scale of the phenomenon, time, and the concentration of impurities. We obtain a family of exact solutions of this problem, which can be regarded as a generalization of the class of linear problems of diffusion considered earlier for the conditions of the ocean and atmosphere by Roberts, Ozmidov, Obukhov,et al. Translated by Peter V. Malyshev and Dmitry V. Malyshev.     

Basic regularities of the process of sedimentation of suspended organic matter in the shallow-water zones of the seas at middle latitudes

On the basis of analysis of literature data, we consider the regularities of sedimentation of suspended organic matter in shallow waters. The seasonal variability in sedimentation is demonstrated, and its scheme is constructed involving such classes of organic compounds as suspended amino acids, fatty acids, and hydrocarbons. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Evaluation of the submarine discharge of karst waters in the region of Cape Aiya

For the submarine springs of underground water located in the karst cavities of Cape Aiya, we suggest a solution based on the modification of the model of flow rate of water and application of the formulas of mixing. We also give methodical recommendations helpful for the reliable determination of empirical parameters under thein situ conditions. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Oscillations of the Black Sea sea level in the north part of the coast

We analyze oscillations of the Black Sea level at 43 points in the north part of the coast. At some points, the data of every-day measurements are accumulated for more than 100 years. Actually, at all points with minor exceptions, we observe a general trend toward an increase in the sea level. The amplitude of oscillations of the sea level about the average trend obeys a normal distribution. We determine numerical characteristics of this distribution. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Analysis of the basic classes of organic compounds dissolved in seawater and their behaviour in the estuaries of rivers and coastal zone of the sea

On the basis of the available literature data, we analyze basic classes of organic compounds dissolved in seawater and study the transformations of proteins, carbohydrates, and lipids produced in the process of photosynthesis in seawater and their behaviour in river water and estuaries of the Black Sea. We also discuss the causes and distinctive features of the processes of production and destruction in the Black Sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Vertical structure of geostrophic currents in the fields of density of water and hydrostatic pressure

We analyze geostrophic currents with nonmonotonic vertical profiles, of velocity and present the distributions of the density of water and hydrostatic pressure corresponding to possible types of the vertical kinematic structure. To prove the existence of the indicated complex layered structures, we use, the data of instrumentalin situ measurements of currents in the Black Sea and in the west part of the Tropical Atlantic. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Spatial structure of the southern polar frontal zone of the Atlantic Ocean

On the basis of the many-year-average seasonal data array of temperature and salinity presented on a scale of one-degree averaging, by using a special quantitative criterion, we reveal a climatic frontal zone and determine both its physical and hydrological characteristics (such as the length width, and thickness of the frontal layer and the temperature, salinity, and density gradients) and its geographic coordinates. The many-year average seasonal variability of these characteristics is analyzed. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Generation of internal waves by a barotropic tide in the coastal zone

Within the framework of the linear theory of long waves, we study internal waves generated by a barotropic tide in a two-layer ocean of variable depth taking into account the influence of the Coriolis force. Barotropic waves run over an extended unevenness of the bottom at an arbitrary angle. This unevenness is regarded as a model of the continental slope and shelf. We establish the dependences of the amplitudes of generated internal waves on the angle of incidence of the barotropic tide, topography of the bottom, and stratification. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Relationship between the depth of visibility of Secchi disk and biooptical characteristics of the Black-Sea waters

We present the parameters of empirical relationships between the depth of visibility of Secchi disk and optical and biological characteristics of the Black-Sea surface waters. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Space structure of the climatic discharge frontal zone of the Amazon

On the basis of the data array of many-year average seasonal values of temperature and salinity represented for a one-degree scale of averaging, by using a quantitative criterion, we select the climatic discharge frontal zone of the Amazon, determine its physical and hydrological characteristics: length, width, thickness of the frontal layer, temperature, salinity, and density gradients, and specify its geographical coordinates. We also describe the many-year average interseasonal variability of these characteristics. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Investigation of transformations of barotropic tides in the coastal zone

Within the framework of the linear theory of long waves, we perform the numerical investigation of transformations of a barotropic diurnal tide in the process of its motion from the deepwater region of the sea into the region of continental slope and shelf zone at any angle to the coast line. For a linear profile of the bottom of the continental slope and shelf, we establish dependences of the amplitudes and velocities of waves on the direction of propagation of the tidal wave and the latitude of the place. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Formation of the dome-shaped isosurfaces of physical and chemical characteristics of the Black Sea

On the basis of processing and analysis of the results of many-year observations, we study the process of formation of dome-shaped isosurfaces of hydrological and hydrochemical characteristics for all depths in the Black Sea. We estimate the roles of the intensities of sources and sinks of heat and dissolved substances and the general picture of water circulation, vertical exchange, meso- and small-scale anticyclonic vorticity, and mud and geothermal flows to the preservation of the dome-shaped form of the isosurfaces of these characteristics. Translated by Peter V. Malyshev and Dmitry V. Malyshev.     

Experimental evaluation of the characteristics of vertical mixing in an oceanic thermohalocline on the basis of fine-structure spectra of advection, salt fingers, and small-scale internal waves

We describe a differential approach to the spectral composition of thin thermohaline inhomogeneities in the ocean depending on the mechanisms responsible for their generation and demonstrate the possibilities of this approach in getting realistic hydrophysical results. The statistical classification of fine-structure fluctuations according to their origin is performed on the basis of the joint analysis of the temperature, salinity, and density spectra computed in a section of the vertical profile where the variation of mean gradients of all three parameters is insignificant. On the basis of the constructed mean spectrum of wave elevations, we estimate the dissipative characteristics of the convection of salt fingers and small-scale internal waves. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

A model of the evolution of vertical thermohaline inhomogeneities of an oceanic thermocline taking into account the effects of double diffusion

We construct a numerical model of the evolution of the structure of an oceanic thermocline in the presence of “salt-finger” convection. The model explains the formation of a piecewise homogeneous vertical structure of the temperature and salinity fields in the ocean. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Application of a probabilistic method to the analysis of accumulation of toxic substances by marine organisms

The process of accumulation of toxic substances by marine organisms is studied on the basis of the kinetic theory of systems of macroscopic particles (V. I. Belyaev, 1987). The use of stochastic equations makes it possible to evaluate the degree of accumulation of toxic substances in marine organisms and take into account random variations of their concentrations in marine environments. Translated by Peter V. Malyshev and Dmitry V. Malyshev.     

Generation of long barotropic waves by moving baric disturbances in a system of basins connected by a channel

We consider long barotropic waves in a system of two rectangular basins connected by a channel in the case where waves are generated by the moving region of disturbances of atmospheric pressure passing above one of the basins. By using a numerical model, we compute the characteristics of the wave process for various values of the parameters of this system. The results of numerical calculations are compared with the corresponding characteristics obtained for the case of a closed basin. We also analyze the distinctive features of long-wave processes induced in the presence of the channel. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Surface gravity waves formed in the process of motion of an ellipsoidal body submerged in the liquid

We study the problem of flow around an ellipsoidal body submerged in a liquid half space and obtain the solution for the free wave surface. The results of numerical analysis reveal the existence of a great variety of modes of motion characterized by substantially different shapes of the free surface. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Relatioship between the intensity of tsunami and the location of the epicentre of underwater earthquakes near the continental slope of the South Coast of Crimea

Within the framework of the nonlinear theory of one-dimensional long waves, we performed the numerical analysis of the dependence of the intensity of tsunami on the shelf of the South Coast of Crimea on the location of the epicentre of underwater earthquakes near the continental slope of the basin. The calculations were carried out for the parameters of the model corresponding to the Yalta tsunami of September 12, 1927. It is shown that, for the same magnitude of the earthquake, the smaller the distance from its epicentre to the coastal line, the lower tsunami waves in the coastal zone and the smaller their vertical run-up. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

On the influence of a diurnal baroclinic tide on the diffusion of an impurity

We investigate the influence of baroclinic tidal waves on the diffusion of an impurity spot in a continuously stratified liquid. The equation of turbulent diffusion is solved numerically by taking into account the wave currents. We establish the dependences of the characteristics of the diffusion process on the parameters of the baroclinic wave and the location of the impurity spot. Translated by Peter V. Malyshev and Dmitry V. Malyshev