Hydrological-Morphometric Characteristics of Danube Delta Branches in the Backwater Zone     

Mikhailova  M. V.  Isupova  M. V.  Morozov  V. N. 《Water Resources》2020,47(3):366-373

Water Resources - The relationships between various hydrological and morphometric characteristics of branch channels in the backwater zone are analyzed in the case of the Chilia channel system in...  相似文献   

Mesoscale Variability of the Ocean in the Northern Part of the Weddell Sea     

Morozov  E. G.  Frey  D. I.  Polukhin  A. A.  Krechik  V. A.  Artemiev  V. A.  Gavrikov  A. V.  Kasian  V. V.  Sapozhnikov  F. V.  Gordeeva  N. V.  Kobylyansky  S. G. 《Oceanology》2020,60(5):573-588

Oceanology - Results of a mesoscale survey in the Powell Basin in the northern part of the Weddell Sea are analyzed. The survey included 24 CTD casts (6 × 4) with an interval of six nautical...  相似文献   

TERMO-LR Experiment on the Luna-27 Lander: Study of Thermophysical,Physicomechanical, and Electromagnetic Properties of the Lunar Soil     

Slyuta  E. N.  Marov  M. Ya.  Dunchenko  A. G.  Makovchuk  V. Yu.  Morozov  O. V.  Nazarov  A. I.  Ivanov  V. V.  Pogonin  V. I.  Roskina  E. G.  Safronov  V. V.  Kharlov  B. N.  Tatsiy  L. P. 《Solar System Research》2021,55(5):446-466

Solar System Research - The device is being developed for the TERMO-LR experiment on the Luna-27 lunar lander; it is intended for contact geophysical measurements of various properties of the lunar...  相似文献   

Antarctic Bottom Water Flow through the Eastern Part of the Philip Passage in the Weddell Sea     

Morozov  E. G.  Frey  D. I.  Tarakanov  R. Yu. 《Oceanology》2020,60(5):589-592

Oceanology - Measurements of currents and Antarctic Bottom Water properties overflowing the sill from the Weddell to the Scotia Sea are described. The bottom water overflows the sill of one of the...  相似文献   

Spatial Structure of the Antarctic Water Flow in the Vema Fracture Zone of the Mid-Atlantic Ridge     

D. I. Frey  E. G. Morozov  V. V. Fomin  N. A. Diansky 《Izvestiya Atmospheric and Oceanic Physics》2018,54(6):621-625

  相似文献   

Polygon-70: Data Interpretation in the Light of New Concepts about Internal Waves     

Morozov  E. G. 《Izvestiya Atmospheric and Oceanic Physics》2020,56(4):428-434

Izvestiya, Atmospheric and Oceanic Physics - We analyze our concepts about ocean dynamics and, in particular, internal waves. Our concepts have changed over the 50 years after the Polygon-70...  相似文献   

The Lomonosov Equatorial Undercurrent according to Data Measured with a Shipborne Profiler, 2014–2017     

Demidova  T. A.  Morozov  E. G.  Neiman  V. G. 《Doklady Earth Sciences》2018,482(1):1229-1233

The velocity and structure of the Lomonosov Equatorial Undercurrent of the Atlantic Ocean are determined based on the data measured with a shipborne acoustic profiler from 2014 to 2017. The seasonal variability of this flow is estimated, and the cases of its outcropping to the surface in the spring of the Northern Hemisphere are revealed.

  相似文献   

The 11th General Meeting of the Russian Mineralogical Society—Modern mineralogy from theory to practice and the Fedorov Session 2010     

M. V. Morozov  D. A. Petrov  T. A. Karyakina 《Geology of Ore Deposits》2011,53(8):818-826

An overview is given of scientific program, summaries of oral communications, and a chronicle of the proceedings of the 11th General Meeting of the Russian Mineralogical Society (RMS), which was held together with the traditional Fedorov Session 2010. The winners of the RMS contests and the discoverers of new minerals are named. The results of election of the RMS governing board and honorary RMS members are published, as well as the final resolution of the meeting and decisions of the RMS scientific council.  相似文献   

Circulation in the southwestern part of the Kara Sea in September 2007     

A. G. Zatsepin  E. G. Morozov  V. T. Paka  A. N. Demidov  A. A. Kondrashov  A. O. Korzh  V. V. Kremenetskiy  S. G. Poyarkov  D. M. Soloviev 《Oceanology》2010,50(5):643-656

During cruise 54 of the R/V Akademik Mstislav Keldysh to the southwestern Kara Sea (September 6 to October 7, 2007), a large amount of hydrophysical data with unique spatial resolution was obtained on the basis of measurements using different instruments. The analysis of the data gave us the possibility to study the dynamics and hydrological structure of the southwestern Kara Sea basin. The main elements of the general circulation are the following: the Yamal Current, the Eastern Novaya Zemlya Current, and the St. Anna Trough Current. All these currents are topographically controlled; they flow over the bottom slopes along the isobaths. The Yamal Current begins at the Kara Gates Strait and turns to the east as part of the cyclonic circulation. Then, it turns to the north and propagates along the Yamal coast over the 100-m isobath. The Eastern Novaya Zemlya Current (its core is located over the eastern slope of the Novaya Zemlya Trough) flows to the northeast. Near the northern edge of Novaya Zemlya, it encounters the St. Anna Trough Current, separates from the coast, and flows practically to the east merging with the continuation of the Yamal Current. A strong frontal zone is formed in the region where the two currents merge above the threshold that separates the St. Anna Trough from the Novaya Zemlya Trough and divides the warm and saline Arctic waters from the cooler and fresher waters of the southwestern part of the Kara Sea. This threshold, whose depth does not exceed 100–150 m, is a barrier that prevents the spreading of the Barents Sea and Arctic waters to the southwestern part of the Kara Sea basin through the St. Anna Trough.  相似文献   

Measurements of bottom currents in the western part of the Romanche Fracture Zone on cruises 37 and 38 of the R/V <Emphasis Type="Italic">Akademik Sergey Vavilov</Emphasis>     

E. G. Morozov  R. Yu. Tarakanov  T. A. Demidova  N. I. Makarenko 《Oceanology》2017,57(5):751-752

  相似文献