Vol 64, No 5 (2024)

Физика моря

On the relation of fine layering of a stratified water environment with vertical turbulent mass transfer

Gerasimov V.V., Zatsepin A.G.

Abstract

The results of a laboratory experiment performed to test the fundamental mechanism of fine layering of a stratified fluid during turbulent impact are described and analyzed. A series of experimental runs were carried out with stirring of an aquatic environment with an initially linear vertical salinity gradient using oscillating vertical rods, creating a uniform turbulent impact throughout the entire thickness of the water column. At the same time, in each run regular measurements of electrical conductivity (salinity) profiles were fulfilled and calculations of the vertical salt flux (mass) were carried out. It turned out that in case of a sufficiently large density (salinity) gradient the mass flux is a decreasing function of the density gradient, and this is the main condition for the formation of a fine layering, according to the proposed mechanism. The experimental results confirmed its feasibility. The dependence of the vertical scale of the fine structure on the parameters of stratification and turbulent impact has also been established.

Океанология. 2024;64(5):739-750
pages 739-750 views

Currents and Tides in the Fram Strait and Greenland Sea

Morozov E.G., Frey D.I.

Abstract

Measurements of oceanographic characteristics, currents, and tides in the Fram Strait and the Greenland Sea are analyzed using historical measurement data. Measurements on moorings across the Fram Strait made it possible to estimate the speeds of the East Greenland and West Spitsbergen currents. It is shown that the speeds of these currents are low (within 10 cm/s) and the amplitudes of the speed of tidal currents are two or more times greater. Tidal currents are intensifying on the shelf of Greenland and Spitsbergen. Direct measurements are compared with the University of Oregon barotropic tide model.

Океанология. 2024;64(5):752-764
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Химия моря

Application of statistical data analysis methods for zoning the kara sea waters

Stepanova S.V., Kivva K.K., Polukhin A.A.

Abstract

The Kara Sea has been systematically studied since the beginning of the 20th century. Large amounts of data have been accumulated as a result of both national and international expeditions. Many publications have been devoted to the Kara Sea area zoning in the light of geomorphological, biological, oceanographic aspects of its nature. This paper presents the results of statistical analysis of combination of hydrophysical and hydrochemical data. On its basis, seven regions of the Kara Sea were identified, and for each region the main characteristics are presented and the factors determining them are highlighted. The results can be used to reconstruct the seasonal course of hydrophysical and hydrochemical parameters, as well as to analyze their interannual variability in different areas of the sea in order to study the response to climatic changes.

Океанология. 2024;64(5):765-776
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Dissolved inorganic carbon (δ13С(DIC), [DIC]) in the waters of western part of Bering Sea

Dubinina Е.О., Kossova S.A., Chizhova Y.N., Avdeenko A.S.

Abstract

For the first time, the isotopic composition and concentration of dissolved inorganic carbon in the waters of the western part of the Bering Sea (at the Koryak shelf and Chukotka continental slope, and Commander Islands, depth interval 10–4100 m) have been analyzed. [DIC] values vary from 1900 μmol/kg in the summer waters of the Koryak shelf to 2510 μmol/kg in the deep waters of the Commander Islands area. The value of δ13С(DIC) in productive summer waters exceeds +1‰, and reach +3.08‰ in the Koryak shelf surface waters. The depth of the carbon isotope minimum (–0.7‰) is ≈500 m. The model calculations were made taking into account physical processes (isotopic exchange with atmospheric CO2 and conservative mixing). The calculations show that in the main water column δ13С(DIC) and [DIC] values are controlled by the oxidation of organic substances. The predominance of primary production occurs only in the surface (<20 m) waters of the Bering Sea. Concentrations of DIC increase to depths of ≈1000 m and remain approximately constant (2430 ± 30 μmol/kg), exceeding [DIC] levels in deep Pacific waters. A “physical carbon pump” model in which the main role in the accumulation and redistribution of DIC within the water column is assigned to the winter waters of the Bering Sea is proposed.

Океанология. 2024;64(5):777-791
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Морская биология

Benthic foraminiferal assemblages as indicators of recent environmental conditions in the northeastern east siberian

Ovsepyan E.A., Ovsepyan Y.S., Mitrofanova N.O., Korsun S.A., Rhee T.S., Jin Y.K.

Abstract

Quantitative analyses of species composition and abundance of benthic foraminifers in the surface samples on the submeridional profile in the northeastern East Siberian Sea reveal three assemblages associated to the middle-outer shelf, upper and middle continental slope. Maximum abundance of “living” benthic foraminifers is found near the shelf break which is possibly related to enhanced sea surface bioproductivity. Active dissolution of calcareous microfossils is detected at the shelf area whereas preservation of calcareous tests becomes better with depth. Some micropaleontological and grain-size data indirectly point to the development of compensatory currents on the middle-outer shelf in the East Siberian Sea.

Океанология. 2024;64(5):792-806
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Морская геология

The structure of the upper sediment cover in the central atlantic based on high-resolution seismoacoustic data

Roslyakov A.G., Dmitrevsky N.N., Ananyev R.A.

Abstract

The study is dedicated to the geological interpretation of high-resolution seismoacoustic data acquired in the Central Atlantic during the 60th cruise of the RV Akademik Ioffe. Seismic facies of abyssal plane deposits, contourites, gravitites, and sediment waves have been identified based on specific characteristics of the seismic structure of the upper sediment cover. Geological interpretation was conducted considering the results of lithological studies of sediment cores collected during research cruises of the Shirshov Institute of Oceanology, Russian Academy of Sciences, as well as deep-sea drilling data. The role of gravity-driven processes in the formation of near-surface deposits is most significant in the region adjacent to the continental margin of South America. In the entire study area, bottom currents are considered as one of the main agents of sediment cover formation. They are responsible both for the deposition of contourite drifts and stratified hemipelagic sediments.

Океанология. 2024;64(5):807-816
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Coastal dunes of the maida river esturary area (zimniy coast of the white sea): structure and history of development

Repkina T.Y., Leontiev P.A., Krekhov A.K., Vyatkin E.D., Orlov A.V., Lugovoy N.N., Shilova O.S.

Abstract

In the NE of the Gorlo Strait of the White Sea interpretation of satellite images, geomorphological and ground penetrating radar profiling, aerial photography and topographic survey of coastal terraces and dunes, diatom analysis and 14C dating of sediments were carried out. The patterns of morphodynamics of coastal and aeolian relief have been established. At the mouth of the Maida River were reconstructed relative sea level changes and the sequence of relief evolution over ~3.7 cal ka BP. Сliff-top dunes are formed on the erosive coasts of the Strait, and on the mouth spit of the Maida River is a foredune plaine. The source of sediment supply for coastal dunes is an extensive sediment flow from NE to SW. Sediment input mainly from the scarp erosion (0.5–3.7 m/year) and from the shoreface, and the role of alluvial runoff is insignificant. At the mouth of the Maida River spit and foredunes have been evolve since the end of the Holocene transgression (~3.7–2.3 cal ka BP). The sea level at mean high water at this time was slightly higher (up to ~2.5 m a. s. l.), and coastal processes were significantly more intense than modern ones. Then, against the background of a decrease in sea level and weakening sediment flows, the growth of the spit slowed down. The ancient foredunes were stabilized by vegetation. Aeolian processes have been activated ~2.1 and after ~0.8–0.7 cal ka BP.

Океанология. 2024;64(5):817-832
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Instruments and methods

Study of the PDO index predictability for 1 to 5 years with INMCM5

Aleksandrov M.S., Volodin E.M., Vorobyeva V.V.

Abstract

The Pacific Decadal Oscillation (PDO) index has been calculated using the INMCM5 climate model developed by the Marchuk Institute of Numerical Mathematics, Russian Academy of Sciences. The PDO index correlation with the reanalysis data decreases from about 1.0 in November of the starting year to 0.355 in October of the following year. The model forecast for the PDO index is reliable for the first 2 years, but correlation coefficients decline significantly after that. The inertial forecast is more accurate in the first 2 years and becomes less reliable onward. The correlation coefficient for the model ensemble forecast of the PDO index with its components in the ensemble is greater than the correlation between the ensemble average and the actual PDO index. The INMCM5 climate model is suggested to have potential for considerable improvement in forecasting the PDO.

Океанология. 2024;64(5):833-840
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Информация

Investigations of the western arctic shelf of russia during the cruise 56 of the r/v “akademik nikolaj strakhov”

Nikiforov S.L., Sorokhtin N.O., Ananiev R.A., Dmitrevskiy N.N., Denisova A.P., Luksha V.L., Meshcheriakov N.I.

Abstract

The article discusses the preliminary results of geological and geophysical, geomorphological and hydrophysical investigations in the Barents and Kara Seas during the Cruise 56 of the R/V Akademik Nikolaj Strakhov in 2023.

Океанология. 2024;64(5):841-843
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Investigations of the sediment cover and magnetic anomalies in in the fracture zones of the tropical atlantic during cruise 65 of the r/v “akademik ioffe”

Ivanova Е.V., Borisov D.G., Gavrikov A.V., Ivanenko A.N., Kirillova O.I., Levchenko O.V., Shakhovskoy I.B., Shulga N.A.

Abstract

This paper provides information on the integrated geological and geophysical investigations in the transform faults valleys of the tropical Atlantic (cruise 65 of the R/V Akademik Ioffe), geomagnetic survey and passing observations on waves and quantitative distribution of cetaceans, birds and flying fish in the North Atlantic (cruises 64 and 65 of the R/V Akademik Ioffe) in October–December 2023. The preliminary scientific results are discussed.

Океанология. 2024;64(5):844-846
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Oceanological Research on High Latitude Transects Near the Spitsbergen Archipelago during the Period of Polar Night

Makarevich P.R., Moiseev D.V., Venger M.P., Maksimovskaya T.M., Rumyantseva Z.Y.

Abstract

In November–December 2023, an expedition of the Murmansk Marine Biological Institute of the Russian Academy of Sciences, on board the R/V Dalnie Zelentsy conducted hydrological, hydrochemical, hydrobiological, and radioecological research in the area west of the Spitsbergen archipelago and on the century-old Kola Meridian transect in the Barents Sea. New data on thermohaline conditions, plankton, and radionuclides during the polar night were obtained at 54 oceanographic and hydrobiological stations. Positive water temperature anomalies show continuation of the warm climate cycle in the Barents Sea. The revealed activation of florogenesis in the western Barents Sea is probably caused by advection of Atlantic waters. Based on an analysis of the population structure of Calanus finmarchicus and C. glacialis in the waters of Spitsbergen, a specific feature of seasonal size variability of species in summer and winter was determined.

Океанология. 2024;64(5):847-849
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Oceanological studies of the russian sectors of the baltic sea in the year 2023

Bubnova E.S., Sivkov V.V., Muratova A.A., Mosharov S.A., Korobchenkova K.D., Dudkov I.Y., Mosharova I.V., Polukhin A.A., Aleksandrov S.V., Artamonov A.Y.

Abstract

The environmental monitoring of the Russian sectors of the Baltic Sea was continued through three expeditions t in 2023: the 55th cruise of the P/V “Akademik Sergei Vavilov” (April), the 54th and 55th cruises of the R/V “Akademik Boris Petrov” (November and December, respectively). Seasonal quantitative estimates of hydrological-hydrochemical and hydrobiological parameters, carbon dioxide fluxes at the water-air interface were obtained, and the geological and geomorphological conditions of the study areas were clarified. Influence of the Neva River to the eastern part of the Gulf of Finland was stable in all seasons and could be traced at a distance of up to 30 nautical miles from the Neva Bay. The South-Eastern Baltic bottom layer experienced extensive hypoxia and mosaic euxunia. Significant aeration of bottom waters occurred in December due to the combined influence of seasonal convection and downwelling resulting from a series of storms. In both study areas, high values of integral primary production were obtained in April, which were two orders of magnitude higher than the December values. The concentration of chlorophyll “a”, accordingly, differed by an order of one magnitude. The Gulf of Finland was an emitter of carbon dioxide into the atmosphere, especially in April, while the South-Eastern Baltic absorbed carbon dioxide in April and was an area of weak emissions in November and December.

Океанология. 2024;64(5):850-852
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Expeditionary studies of the seas of north-east eurasia during the 69th cruise of r/v “akademik oparin”

Charkin A.N., Dudarev O.V., Ulyantsev A.S.

Abstract

The paper provides information about the integrated oceanological studies in the Bering, Chukchi and East Siberian Seas during the 69th cruise of R/V “Akademik Oparin” in September–October 2023. Preliminary results of the scientific expedition are discussed.

Океанология. 2024;64(5):853-855
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Studies of waters off the western coast of the novaya zemlya archipelago during a cruise with r/v “dalnie zelentsy” in august 2023

Makarevich P.R., Ezhov A.V., Bondarev O.V., Venger M.P., Karamushko O.V., Moskvin K.K., Raskhozheva E.V.

Abstract

Integrated marine investigations were carried out by researchers at the Murmansk Marine Biological Institute of the Russian Academy of Sciences during a cruise in August 2023 on r/v “Dalnie Zelentsy” within the national project called “Science and Universities”. The investigations included CTD sampling, hydrologic, hydrochemic, hydrobiologic, ichthyologic, and radioecologic studies, and observations of marine birds and mammals. The outcome of the cruise was new data on the reference state of the ecosystem of the eastern Barents Sea.

Океанология. 2024;64(5):856-859
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Gas geochemical studies of amur and ussuri bays (sea of japan) on the r/v “professor gagarinskiy”, cruises № 84, 85

Yatsuk A.V., Bovsun M.A., Shakirov R.B., Kalinchuk V.V., Makseev D.S., Yugai I.G., Shvalov D.A., Sigeev I.A., Aksentov K.I., Maltseva E.V., Lazaryuk A.Y.

Abstract

Information is provided on the results of gas geochemical and hydrometeorological studies of the Amur and Ussuri bays, the Sea of Japan on cruises 84 and 85 of the R/V “Professor Gagarinskiy” in December 2022. For the first time for the winter period, synchronous measurements of greenhouse gases and atomic mercury were carried out in the surface marine boundary layer of Peter the Great Bay, and new information was obtained on the seasonal characteristics of gas geochemical fields in the water column and bottom sediments.

Океанология. 2024;64(5):860-862
pages 860-862 views

Study of oceanographic conditions in the area of the avachinskiy bay of kamchatka in winter in the expedition on the r/v “akademik oparin” (cruise no. 65)

Lobanov V.B., Sergeev A.F., Semkin P.Y., Lukyanova N.B., Goryachev V.A., Sagalaev S.G., Tsoy V., Alekseev I.F., Barabanshchikov Y.A., Kalyuzhniy D.S., Kushnir P.G., Mazur A.A., Prushkovskaya I.A., Razzhivin V.V., Ryumina A.A., Sokolov D.D., Ulanova O.A., Shkirnikova E.M.

Abstract

During the cruise No. 65 of the R/V “Akademik Oparin”, which was carried out from November 26 to December 29, 2022, research was continued in the area of the Avachinskiy Bay of Kamchatka to study the possible factors that caused the mass moratlity of marine organisms in the Fall of 2020, and complex hydrographic and hydrochemical surveys on the northeastern shelf of Sakhalin Island to monitor the environmental situation in areas of oil and gas production and in the southern part of the Sea of Okhotsk. According to data from two autonomous moorings deployed in the coastal zone of Avachinskiy Bay with an exposure of 169 days, relatively calm water dynamics in the bay were noted throughout the entire Summer-Fall season of 2022, which contributed to the enrichment of waters with nutrients necessary for the development of plankton. No noticeable decrease in oxygen content was recorded. A survey of the southern part of the East Kamchatka Current was carried out, the evolution and the structure of the anticyclonic eddy of the Avachinskiy Bay at the moment of its splitting were traced. Hydrochemical characteristics of coastal bays and rivers during the freeze-up period were studied. Samples of plankton and bottom sediments were taken for special analyzes in the laboratories of the Pacific Institute of Bioorganic Chemistry and the National Center for Marine Biology of Far Eastern Branch of the Russian Academy of Sciences.

Океанология. 2024;64(5):863-866
pages 863-866 views