Horizontal and Vertical Structure of Geostrophic Currents in the Black Sea According to the Data of the Summer Survey Performed as a Part of the ComSBlack-92 Program

We describe the methodology and software developed for the numerical analysis of the characteristics of the horizontal and vertical structure of geostrophic currents. We present the results of computation of these characteristics according to the data of the summer survey of the Black Sea carried out as a part of the ComSBlack-92 program. The distinctive features of the space structure of geostrophic currents discovered as a result and the established parameters of their variability may supplement the existing data on the current field in the Black Sea.     

The dynamic method of calculating currents and analysis of the vertical kinematic structure

The basic relations of the classical dyamic method have been complemented with the condition allowing for the non-monotonicity of the vertical kinematic structure. The elements of the multi-layered system of geostrophic currents have been found to correlate over depth with seawater density and hydrostatic pressure distribution. An example of the analysis of the vertical structure of currents, involving specific hydrological data, is given. Translated by Vladimir A. Puchkin.     

Large-scale vertical hydroacoustic structure of the North Atlantic and its seasonal variability

A classification based on the number and types of large-scale acoustic waveguides is proposed for the mean seasonal profiles of sound speed propagation. A scheme for North Atlantic zoning, using typical curves of the sound speed vertical distribution, is given. The channel axis's position is shown not to depend on the water mass haline properties, being controlled by the temperature field vertical stratification.Translated by Vladimir A. Puchkin.     

Physical and hydrological characteristics of climatic frontal zones in the Tropical Atlantic

Climatic frontal zones are selected in the thermohaline fields of the Tropical Atlantic by analyzing the many-year-average seasonal database reduced to the nodes of a one-degree grid. We determine physical characteristics of the frontal zones, study their spatial and temporal variability, and reveal basic regularities of the appearance of frontal zones in the fields of thermohaline characteristics. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

North Brazil current: vertical structure

On the basis of the data ofin situ measurements of the velocities of currents and basic hydrophysical parameters (such as temperature and salinity) carried out during Cruise 41 of the R/VAkademik Vernadsky, we analyze the structure of the North Brazil Current near the continental slope and in the equatorial abyssal part of the ocean in winter, establish the regularities of changes in the current velocity with depth, and compare the structures of the North Brazil and Guiana Currents. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Bioestimation: A new method for the control of water self-purification process and its comparison with bioindication

A new line in the studies of water bodies is proposed: the assessment and correction of the process of biotic purification of water (biological treatment and self-purification). The proposed approach is based on a principally new hydrobiological method of monitoring and control of water quality formation process—bioestimation. The principal novelty of bioestimation is due to the fact that it controls not the quality of the aquatic medium, but the object that has not been controlled before—water purification process and organic matter transformations in the process of vital activity of saprotrophic bacteria. Three critical groups of factors were found to govern the activity of these bacteria: the dynamic characteristics of the aquatic environment; the load on destructors in terms of organic matter; and the impact of substances, which are atypical of natural water and most often are discharged in it with industrial wastes. A group of indicator microorganisms—bioestimators—is chosen for each group of factors. The population size of such estimators can be used to identify and next eliminate the disturbing factor. The bioestimators are not species but ecological groups of microorganisms, commonly inhabiting any waters, either salt or fresh. Bioestimation also helps to identify disturbances in water purification process even in the cases where analyses of aquatic environment quality do not signal alarm. The proposed method is described and its major distinctions from the well-known hydrobiological method (bioindication in its original, saprobiological meaning) are demonstrated.     

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     

Mean current velocity measurement from a movable base

This paper discusses the possibility of measurement of the current velocity vector characteristics averaged over the time of continuous regular down-up probings from a moving carrier. The measurements can be carried out either from a moving vessel or from a helicopter, floating on or hovering above the sea surface. As an illustration for the suggested technique,in situ observations compiled by a free-component (±XYZ) VEGA-3 probe in the Guiana current region in March 1990 are provided. Comparison of the results with buoy data shows good agreement within the accuracy limits of the instruments employed.Translated by Vladimir A. Puchkin.     

Vertical hydroacoustic structure of the Tropical Atlantic central and intermediate waters

Large-scale CTD survey data are used to calculate the acoustic velocity in the North Tropical Atlantic. It has been stated that a characteristic feature of the vertical hydroacoustic structure in this region is associated with the presence of numerous local sound channels in the subsurface and intermediate layers. Characteristics of these channels are given and possible causes of their origin are discussed. It is shown how local acoustic waveguides affect the sound beam trajectory.Translated by V. Puchkin.     

Hydrometeorological conditions in the north-eastern Arabian Sea shelf zone during the period of the trade winds' change and their impact on the formation of commercial fish shoals

This paper examines the oceanographic situation in the north-eastern Arabian Sea shelf area during the period when the trade winds change. The location and intensity of the discharge front there have been found to be dictated by tidal events and the wind régime. It is shown that commercial fish shoals move over the water column along with the front and that fish catches are largest when the front is steady.Translated by Vladimir A. Puchkin.