DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS最新文献_第2页

ON EVALUATION OF THE ROLE OF THERMAL AND WIND FACTORS FOR A PHYSICAL MODEL OF THE WORLD OCEAN GENERAL CIRCULATION SYSTEM 热因子和风因子对世界海洋环流系统物理模式的作用评价

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).7

В.Г. Нейман, О Роли, Термического И Ветрового, Факторов В Физической, Модели Общей, Циркуляция Вод, Мирового океана, Нейман В.Г

{"title":"ON EVALUATION OF THE ROLE OF THERMAL AND WIND FACTORS FOR A PHYSICAL MODEL OF THE WORLD OCEAN GENERAL CIRCULATION SYSTEM","authors":"В.Г. Нейман, О Роли, Термического И Ветрового, Факторов В Физической, Модели Общей, Циркуляция Вод, Мирового океана, Нейман В.Г","doi":"10.29006/1564-2291.jor-2019.47(3).7","DOIUrl":"https://doi.org/10.29006/1564-2291.jor-2019.47(3).7","url":null,"abstract":"The main content of the work consists of certain systematization and addition of longexisting, but eventually deformed and partly lost qualitative ideas about the role of thermal and wind factors that determine the physical mechanism of the World Ocean’s General Circulation System (OGCS). It is noted that the conceptual foundations of the theory of the OGCS in one form or another are contained in the works of many well-known hydrophysicists of the last century, but the aggregate, logically coherent description of the key factors determining the physical model of the OGCS in the public literature is not so easy to find. An attempt is made to clarify and concretize some general ideas about the two key blocks that form the basis of an adequate physical model of the system of oceanic water masses motion in a climatic scale. Attention is drawn to the fact that when analyzing the OGCS it is necessary to take into account not only immediate but also indirect effects of thermal and wind factors on the ocean surface. In conclusion, it is noted that, in the end, by the uneven flow of heat to the surface of the ocean can be explained the nature of both external and almost all internal factors, in one way or another contributing to the excitation of the general, or climatic, ocean circulation.","PeriodicalId":169855,"journal":{"name":"DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127829364","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

INVESTIGATION OF THE MECHANISMS OF GENERATION OF SEA SPRAYS DURING STRONG WINDS, THEIR ROLE IN THE MECHANICS AND THERMODYNAMICS OF HURRICANES 研究强风中海雾的产生机制及其在飓风力学和热力学中的作用

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).14

Y. Troitskaya, O. Druzhinin, O. Ermakova, A. Kandaurov, D. Kozlov, D. Sergeev

引用次数: 0

COLLISION OF THE DROPLET WITH THE FREE SURFACE: ACOUSTIC EMISSION IN THE WATER COLUMN 液滴与自由表面的碰撞:水柱中的声发射

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).10

Victor Prokhorov

引用次数: 0

VARIABILITY OF THE THERMOHALINE STRUCTURE AT THE CONTINENTAL SLOPE OFF THE RUSSIAN COAST, THE NORTHWESTERN JAPAN SEA 日本海西北部俄罗斯海岸外大陆斜坡温盐构造的变化

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).15

O. Trusenkova, A. G. Ostrovskii, A. Lazaryuk, V. Lobanov

{"title":"VARIABILITY OF THE THERMOHALINE STRUCTURE AT THE CONTINENTAL SLOPE OFF THE RUSSIAN COAST, THE NORTHWESTERN JAPAN SEA","authors":"O. Trusenkova, A. G. Ostrovskii, A. Lazaryuk, V. Lobanov","doi":"10.29006/1564-2291.jor-2019.47(3).15","DOIUrl":"https://doi.org/10.29006/1564-2291.jor-2019.47(3).15","url":null,"abstract":"The study is based on unique data from the autonomous Aqualog profiler installed in the northwestern Japan Sea at the continental slope off the southeastern Primorye coast from April 18 through October 14, 2015. Data set for the 64–300 m depths, with the depth step of 1 m and time step of 6 hours, and the time series averaged for the 320–420 m depths, with the time step of 6 days, are used. Variability in the upper and lower profiled layers is found to be of different nature. Above 100–150 m short-lived (2–4 days) temperature and salinity anomalies are mostly of the same sign. Based on our earlier analysis of satellite information it is possible to link these anomalies with water intrusions of different origins. Conversely, these anomalies are usually of the opposite signs and are longer-lived (up to 10–15 days) in the lower layer which can be explained by vertical displacements of isopycnals, probably due to passing mesoscale and submesoscale disturbances. Based on wavelet transform it is found that the longest-period fluctuations (with the periods of 80–110 days) were the most intense in the entire profiled layer throughout the entire record. Isopycnal displacements with the periods of 80–110 days were also found, being in-phase with the temperature fluctuations. The wavelet transform also revealed that variability strengthened in the upper layer and weakened in the lower layer from mid-August onwards.","PeriodicalId":169855,"journal":{"name":"DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS","volume":"8 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134515590","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

LONG-PERIOD VARIABILITY OF LARGE-SCALE CIRCULATION SYSTEM AND MESOSCALE VORTICES AS SELF-ORGANIZATION PHENOMENON 作为自组织现象的大尺度环流系统和中尺度涡的长周期变率

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).16

A. Fedotov

引用次数: 0

FORMATION OF THE COLD INTERMEDIATE LAYER IN THE SHELF-SLOPE NORTHEASTERN PART ZONE OF THE BLACK SEA 黑海东北部陆架斜坡带冷中间层的形成

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).5

S. Kuklev, A. Zatsepin, O. Podymov

引用次数: 3

SEASONAL VARIABILITY OF OCEANOLOGICAL CONDITIONS ON THE NORTHEASTERN SAKHALIN SHELF BASED ON THE SURVEYS ON STANDARD SECTIONS 基于标准剖面调查的东北库页岛陆架海洋条件的季节变化

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).19

G. Shevchenko, V. Chastikov

{"title":"SEASONAL VARIABILITY OF OCEANOLOGICAL CONDITIONS ON THE NORTHEASTERN SAKHALIN SHELF BASED ON THE SURVEYS ON STANDARD SECTIONS","authors":"G. Shevchenko, V. Chastikov","doi":"10.29006/1564-2291.jor-2019.47(3).19","DOIUrl":"https://doi.org/10.29006/1564-2291.jor-2019.47(3).19","url":null,"abstract":"The long-term mean temperature and salinity distributions on 5 standard oceanological sections on the northeast shelf of Sakhalin were analyzed for 4 months of the navigation period (July-October) including a radical restructuring of hydrological conditions in the transition from summer to autumn. The data of soundings performed during the pollock ichthyoplankton surveys were used to study oceanological conditions in June. The low salinity water formed by the Amur River runoff are shown to appear on the northeastern shelf in the first half of June after the heavy ice breaking in the southern Sakhalin Bay. Low salinity water and ice are pushed off toward the deep sea under the influence of the southern winds typical for a warm season, and an oceanological front is formed near the 52°N. This front prevents the low-salinity water from flowing southward until the second half of September, when changes into a winter monsoon with the prevailing northerly winds take place. This promotes destruction of hydrological front and deepening of the cold intermediate water layer. The waters with the 4–6°C temperature and salinity of about 31 psu occur at the shelf edge along the northeastern Sakhalin coast. A powerful stream with the relatively warm low salinity water is being formed along the shore that reaches the southeastern part of Sakhalin and northern coasts of Hokkaido Island.","PeriodicalId":169855,"journal":{"name":"DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS","volume":"80 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114804431","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

SELF-EXCITED OSCILLATIONS IN THE DRIFTING ICE COVER OF THE ARCTIC OCEAN 北冰洋漂流冰盖的自激振荡

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2019-11-06 DOI: 10.29006/1564-2291.jor-2019.47(3).11

V. Smirnov, S. Kovalev, A. A. Nubom

引用次数: 5

ON THE ROLE OF MESOSCALE VORTICES IN THE OIL SPILL TRANSPORT IN THE SOUTH-EASTERN BALTIC SEA (SATELLITE INFORMATION) 中尺度涡旋在波罗的海东南部溢油运输中的作用(卫星资料)

DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS Pub Date : 2018-11-02 DOI: 10.29006/978-5-9901449-4-1-2018-24

A. Ginzburg, E. Krek, A. Kostianoy, D. M. Soloviev

{"title":"ON THE ROLE OF MESOSCALE VORTICES IN THE OIL SPILL TRANSPORT IN THE SOUTH-EASTERN BALTIC SEA (SATELLITE INFORMATION)","authors":"A. Ginzburg, E. Krek, A. Kostianoy, D. M. Soloviev","doi":"10.29006/978-5-9901449-4-1-2018-24","DOIUrl":"https://doi.org/10.29006/978-5-9901449-4-1-2018-24","url":null,"abstract":"In this paper, on the basis of an analysis of the successive satellite optical images (MODISAqua, TIRS Landsat-8, AVHRR NOAA-18) and radar images (SAR-C Sentinel-1A, SAR-C Radarsat-2) on June 8–11, 2015, the effect of the mesoscale vortex movement (anticyclone with diameter of 35 km and associated cyclone) on the transport of oil spots in the northern part of the Gdansk Bay was demonstrated for the first time. The velocities of this transport are estimated; the observed picture of the movement of the spots is compared with their transfer according to the Seatrack Web model. The largest (about 20 cm/s) drift velocity corresponded to the spot that appeared near the periphery of the anticyclonic vortex (the region of maximum velocities), the smallest one was at the spot near the center of the vortex. At a wind speed of not more than 5 m/s on June 10 and an assumed orbital velocity of the anticyclone of the order of 20 cm/s, the contribution of the vortex motion to the total transport of the spots under the influence of wind and vortex should be decisive. The observed drift of the spots did not correspond to the forecast of their movement by the Seatrack Web numerical model, which did not take into account the vortex dynamics of the waters.","PeriodicalId":169855,"journal":{"name":"DEDICATED TO THE 90TH ANNIVERSARY OF PROF. K.N. FEDOROV OCEAN PHYSICS","volume":"7 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121780642","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1