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951.
952.
The paper is concerned with the evaluation of the drift current parameters derived through the use of an analytical model.
In this model, effective when stratification is stable and indifferent, the vertical turbulence coefficient profile is prescribed
by the power function, and hydrodynamic quantities are prescribed using the external parameters of the problem (wind stress,
the Coriolis parameter, and the dimensionless stratification parameter). Model data are compared with the observations of
the upper mixed layer in the vicinity of the oceanic Station C, conducted during one year. It is shown that, under the spring-summer-time
warming conditions, the model at issue is capable of adequately simulating the upper ocean layer dynamics.
Translated by Vladimir A. Puchkin. 相似文献
953.
In application to the Crimean regional centre for satellite data reception, treatment, and dissemination, we have identified
the earth’s satellite-surveyed areas, with orbital heights (H) ranging from 650 to 750 km. This paper shows that for the Ukrainian territory and the Sea of Azov-Black Sea environment
to be monitored, the regional centre’s receiving station must be capable of receiving radar signals from a range of about
1500 km. For typical high-speed radio lines, this may be achieved through the use of a satellite data-receiving station, with
the antenna’s diameter being about 3 m.
Translated by Vladimir A. Puchkin. 相似文献
954.
V. N. Kudryavtsev 《Physical Oceanography》1996,7(2):99-125
This paper discusses a simplified model for the evolution of the atmospheric planetary boundary layer overlying a thermal
front in the sea. The model provides local values of the friction/heat transfer geostrophic coefficients and the direction
of surface wind stress, as well as the wind/temperature profiles at any point on the front. With the running over a warm front,
the baroclinicity of the internal boundary layer leads to the generation of a near-surface current of air directed down the
front. The model can be used to interpret radar imagery of the sea surface with the purpose of determining its mesoscale variability.
Translated by Vladimir A. Puchkin. 相似文献
955.
This paper discusses the application of acoustic sounding with the purpose of identifying vortical features in the sea. Analysis
of the results of a multidisciplinary acoustic/hydrological experiment conducted in the Black Sea has revealed a stable recurrent
correlation between the amplitudinal variance of echo signals, on the one hand, and the peculiarities of water temperature
fields, on the other. Given these characteristics, the peripheral and the central areas of a mesoscale eddy essentially differed.
This allows us to apply acoustic sounding to identify mesoscale eddies in the sea.
Translated by Vladimir A. Puchkin. 相似文献
956.
957.
958.
959.
This paper deals with the solution of the problem of the dynamic response of the leg of a tension leg platform subjected to an axial, suddenly applied load at one end, considering a highly simplified model but taking into account several complicating factors. The problem is solved by means of a non-harmonic Fourier expansion in terms of eigenfunctions obtained from a non-regular Sturm-Liouville system. 相似文献
960.
P. Dewangan T. RamprasadM.V. Ramana A. MazumdarM. Desa F.K. Badesab 《Marine and Petroleum Geology》2010
Increased oil and gas exploration activity has led to a detailed investigation of the continental shelf and adjacent slope regions of Mahanadi, Krishna–Godavari (KG) and Cauvery basins, which are promising petroliferous basins along the eastern continental margin of India. In this paper, we analyze the high resolution sparker, subbottom profiler and multibeam data in KG offshore basin to understand the shallow structures and shallow deposits for gas hydrate exploration. We identified and mapped prominent positive topographic features in the bathymetry data. These mounds show fluid/gas migration features such as acoustic voids, acoustic chimneys, and acoustic turbid layers. It is interesting to note that drilling/coring onboard JOIDES in the vicinity of the mounds show the presence of thick accumulation of subsurface gas hydrate. Further, geological and geochemical study of long sediment cores collected onboard Marion Dufresne in the vicinity of the mounds and sedimentary ridges shows the imprints of paleo-expulsion of methane and sulfidic fluid from the seafloor. 相似文献