Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Vladimir Rogozhin"'
Autor:
Alina Demkina, Darya Slonova, Viktor Mamontov, Olga Konovalova, Daria Yurikova, Vladimir Rogozhin, Vera Belova, Dmitriy Korostin, Dmitry Sutormin, Konstantin Severinov, Artem Isaev
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-18 (2023)
Abstract Metagenomics is a powerful tool to study marine microbial communities. However, obtaining high-quality environmental DNA suitable for downstream sequencing applications is a challenging task. The quality and quantity of isolated DNA heavily
Externí odkaz:
https://doaj.org/article/d140a6244af748aebcc9cbd46c6b5d86
Autor:
Alexander Osadchiev, Roman Sedakov, Dmitry Frey, Alexandra Gordey, Vladimir Rogozhin, Zinaida Zabudkina, Eduard Spivak, Ekaterina Kuskova, Andrey Sazhin, Igor Semiletov
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-10 (2023)
Abstract The Kara Sea receives ~ 1/3 of total freshwater discharge to the Arctic Ocean, mainly from the large Ob and Yenisei rivers. The Ob-Yenisei plume covers wide area in the central part of the Kara Sea during ice-free season (June–October) and
Externí odkaz:
https://doaj.org/article/aeda07ebacb74d9fb4faa29303acf2db
Autor:
Alexander Osadchiev, Zinaida Zabudkina, Vladimir Rogozhin, Dmitry Frey, Alexandra Gordey, Eduard Spivak, Anatoly Salyuk, Igor Semiletov, Roman Sedakov
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
The major Siberian rivers form large river plumes in the Arctic Ocean, which govern structure of the sea surface layer at the Arctic shelf. These river plumes were explicitly studied during the warm period in summer and early autumn characterized by
Externí odkaz:
https://doaj.org/article/66d40ce9369e47a7b71a90fdaaf4259c
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
The Pechora River forms the large Pechora River plume in the southeastern part of the Barents Sea (also called the Pechora Sea). Many previous works addressed water masses in the Barents Sea, however, the Pechora plume received relatively little atte
Externí odkaz:
https://doaj.org/article/a935e688019145888479b584a3734c40
Publikováno v:
Remote Sensing, Vol 15, Iss 13, p 3397 (2023)
Wind is the main external force that governs the spreading of river plumes in the sea. Many previous studies demonstrated that the spreading direction of river plumes (especially small plumes) generally coincides with wind direction. At the same time
Externí odkaz:
https://doaj.org/article/29edcf3565af44ebb28207448b028d1c
Autor:
Alexander Osadchiev, Alexandra Gordey, Alexandra Barymova, Roman Sedakov, Vladimir Rogozhin, Roman Zhiba, Roman Dbar
Publikováno v:
Remote Sensing, Vol 14, Iss 15, p 3818 (2022)
The interfaces between small river plumes and ambient seawater have extremely sharp horizontal and vertical salinity gradients, often accompanied by velocity shear. It results in formation of instabilities at the lateral borders of small plumes. In t
Externí odkaz:
https://doaj.org/article/ca5866b5161945e4bc8f8d33ad4fa8b5
Publikováno v:
Computer Science Journal of Moldova, Vol 12, Iss 1(34), Pp 80-88 (2004)
In computational processes based on backwards chaining, a rule of the type is seen as a procedure which points that the problem can be split into the problems. In classical devices, the subproblems are solved sequentially. In this paper we present so
Externí odkaz:
https://doaj.org/article/3dfb30fdf3f34f26a8fed7391aa7cf33
Autor:
Anna Gebruk, Polina Dgebuadze, Vladimir Rogozhin, Yulia Ermilova, Nikolay Shabalin, Vadim Mokievsky
Publikováno v:
Polar Biology. 46:473-487
The Pechora Bay is a hydrologically and ecologically important area of the Barents Sea but there are still gaps in our knowledge of biodiversity of the area, including macrozoobenthos. In the first half of the twentieth century, the Pechora Bay was n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad7ceac035a8f7c7cd94f582c7b27266
https://doi.org/10.1007/s00300-023-03138-4
https://doi.org/10.1007/s00300-023-03138-4
Autor:
Vladimir Rogozhin, Alexander Osadchiev
The Barents Sea is a shelf marginal sea of the Arctic Ocean. The river runoff in the Barents Sea is small (260 km3 per year) and does not have a significant effect on hydrophysical processes with the exception of the southeastern part of the sea, whe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fd2d0082a9210725fac8ddb40196092
https://doi.org/10.5194/egusphere-egu22-7299
https://doi.org/10.5194/egusphere-egu22-7299
The annual runoff of river water into the Laptev Sea is 745 km3, most of the runoff belongs to the Lena River - 525 km3. Long-term variability in the volume of the Lena River runoff play a significant role in the variability of the scale of distribut
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20786b197cd5734c84ec29d89b38ac09
https://doi.org/10.5194/egusphere-egu21-14630
https://doi.org/10.5194/egusphere-egu21-14630