Zobrazeno 1 - 10
of 29
pro vyhledávání: '"I. A. Zhabin"'
Publikováno v:
Известия ТИНРО, Vol 192, Iss 1, Pp 177-183 (2018)
Data of observations on drifters in 1988–2015 are used to study seasonal variability of the surface water circulation in the Japan Sea. The well-known circulation patterns are observed, as the Tsushima Current, the East-Korean Current, the Primorye
Externí odkaz:
https://doaj.org/article/0f3e1b9179e14011874824846f72a486
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 58:1438-1449
Autor:
I. A. Zhabin, N. B. Luk’yanova
Publikováno v:
Russian Meteorology and Hydrology. 47:660-667
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 57:1627-1642
Autor:
I. A. Zhabin, E. V. Dmitrieva
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 57:1680-1689
Autor:
N. B. Luk’yanova, I. A. Zhabin
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 56:1615-1620
Images in the visible range of the MODIS Terra/Aqua and ETM+ Landsat 7/OLI Landsat 8 satellites are used to study vortex streets (VSes) in the region of the Shantar Islands (Sea of Okhotsk). Two stable VSes are observed in the Northeast Strait
Autor:
I. A. Zhabin, A. G. Andreev
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 55:1114-1124
We have investigated the interaction between the mesoscale and submesoscale eddies in the deep Kuril Basin of the Sea of Okhotsk. An analysis of the long-term series of satellite altimetry observations (2000–2011) has demonstrated that the circulat
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 55:1172-1181
The Shantar Islands National Park (northwestern shelf of the Sea of Okhotsk) was established to preserve the biological diversity of unique natural marine and terrestrial ecosystems. The water structure and dynamics in the basin of the Shantar Island
Publikováno v:
Russian Meteorology and Hydrology. 44:130-135
The response of the thermohaline structure of water off the western Kamchatka shelf of the Sea of Okhotsk to the wind-driven upwelling and tidal mixing is analyzed, and the results are presented. The upwelling intensity was estimated based on the off