Zobrazeno 1 - 10
of 14
pro vyhledávání: '"A. N. Salyuk"'
Autor:
I. I. Pipko, S. P. Pugach, I. P. Semiletov, L. G. Anderson, N. E. Shakhova, Ö. Gustafsson, I. A. Repina, E. A. Spivak, A. N. Charkin, A. N. Salyuk, K. P. Shcherbakova, E. V. Panova, O. V. Dudarev
Publikováno v:
Ocean Science, Vol 13, Pp 997-1016 (2017)
The Arctic is undergoing dramatic changes which cover the entire range of natural processes, from extreme increases in the temperatures of air, soil, and water, to changes in the cryosphere, the biodiversity of Arctic waters, and land vegetation.
Externí odkaz:
https://doaj.org/article/7151962f724c44a1a1a8b7a6b21fcfcf
Autor:
A. N. Charkin, M. Rutgers van der Loeff, N. E. Shakhova, Ö. Gustafsson, O. V. Dudarev, M. S. Cherepnev, A. N. Salyuk, A. V. Koshurnikov, E. A. Spivak, A. Y. Gunar, A. S. Ruban, I. P. Semiletov
Publikováno v:
The Cryosphere, Vol 11, Pp 2305-2327 (2017)
It has been suggested that increasing terrestrial water discharge to the Arctic Ocean may partly occur as submarine groundwater discharge (SGD), yet there are no direct observations of this phenomenon in the Arctic shelf seas. This study tests the
Externí odkaz:
https://doaj.org/article/e4905923875c40c59388689fbfd39692
Autor:
Natalia Shakhova, Irina I. Pipko, Elena Panova, Kseniia P. Shcherbakova, Oleg Dudarev, Leif G. Anderson, Igor Semiletov, Eduard A. Spivak, A. Charkin, Irina Repina, Anatoly N. Salyuk, Svetlana P. Pugach, Örjan Gustafsson
Publikováno v:
Ocean Science. 13:997-1016
The Arctic is undergoing dramatic changes which cover the entire range of natural processes, from extreme increases in the temperatures of air, soil, and water, to changes in the cryosphere, the biodiversity of Arctic waters, and land vegetation. Sma
Autor:
Alexander N. Charkin, Michiel Rutgers van der Loeff, Natalia E. Shakhova, Örjan Gustafsson, Oleg V. Dudarev, Maxim S. Cherepnev, Anatoly N. Salyuk, Andrey V. Koshurnikov, Eduard A. Spivak, Alexey Y. Gunar, Igor P. Semiletov
It has been suggested that increasing freshwater discharge to the Arctic Ocean may also occur as submarine groundwater discharge (SGD), yet there are no direct observations of this phenomenon in the Arctic shelf seas. This study tests the hypothesis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f908db94a62e1a3554522c48256d7439
https://doi.org/10.5194/tc-2017-33
https://doi.org/10.5194/tc-2017-33
Autor:
Alexander N. Charkin, Michiel Rutgers van der Loeff, Natalia E. Shakhova, Örjan Gustafsson, Oleg V. Dudarev, Maxim S. Cherepnev, Anatoly N. Salyuk, Andrey V. Koshurnikov, Eduard A. Spivak, Alexey Y. Gunar, Igor P. Semiletov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81bed33b5cf61586e8a87fa52bfb6c17
https://doi.org/10.5194/tc-2017-33-supplement
https://doi.org/10.5194/tc-2017-33-supplement
Publikováno v:
Russian Meteorology and Hydrology. 37:254-260
Hydrological flow front whose location and structure depend on the value of the Lena River water flow forms in winter under the ice in the Buor-Khaya Bay. The flow front is characterized by the baroclinic and thermocline components. Under the lens of
Publikováno v:
Oceanology. 50:869-876
The thermohaline and hydrochemical characteristics of the Lena River’s estuarine zone were investigated in the Buor-Khaya Bay and the southeastern Laptev Sea in September of 2005. A tongue of river water with high nutrient content and increased tur
Publikováno v:
Russian Meteorology and Hydrology. 33:106-111
The field data show that the ventilation of waters in the Sea of Okhotsk occurs the year round as a cyclic process and consists of several phases. During the initial phase, the shelf waters enter the offshore subsurface layers. Later, they appear at
Publikováno v:
Russian Meteorology and Hydrology. 32:50-53
Data of field observations are indicative of the periodic appearance of intrusions of cold water at depths of 250–400 m near the northeastern Sakhalin continental slope in summer. Monitoring of the oceanographic conditions in the area shows that th
Autor:
Walter C. Oechel, Donatella Zona, Paulo C. Olivas, Steven F. Oberbauer, A. N. Salyuk, John Kochendorfer, David A. Lipson
Publikováno v:
Global Biogeochemical Cycles. 23
[1] Much of the 191.8 Pg C in the upper 1 m of Arctic soil of Arctic soil organic mater is, or is at risk of, being released to the atmosphere as CO2 and/or CH4. Global warming will further alter the rate of emission of these gases to the atmosphere.