Zobrazeno 1 - 10
of 14
pro vyhledávání: '"R. Yu. Gnatovskii"'
Publikováno v:
Water Resources. 49:184-192
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02089c7754892d5221b28d21af1f72a4
https://doi.org/10.1134/s0097807822020075
https://doi.org/10.1134/s0097807822020075
Publikováno v:
Russian Meteorology and Hydrology. 44:674-678
Changes in the ionic component of the under-ice mineralization in the southern basin of Lake Baikal in 2001–2016 are analyzed. Data on the under-ice layer mineralization variations derived from water conductivity measurements using the SBE-25 high-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aac9cd60f343de2f4edb008d30ce8ae5
https://doi.org/10.3103/s1068373919100054
https://doi.org/10.3103/s1068373919100054
Autor:
V. V. Blinov, V. G. Ivanov, R. Yu. Gnatovskii, Valery V. Kozlov, N. G. Granin, I. B. Mizandrontsev, K. M. Kucher, A. A. Zhdanov, E. A. Tsvetova, I.A. Aslamov
Publikováno v:
Russian Geology and Geophysics. 59:1514-1525
Hydrophysical studies and mathematical modeling of ring structures during ice cover on Lake Baikal have shown that their existence at the stage of ice cover degradation is due to anticyclonic currents. Such currents can be generated as a result of lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d32e894d3201be2a95875b35377f16a2
https://doi.org/10.1016/j.rgg.2018.10.011
https://doi.org/10.1016/j.rgg.2018.10.011
Publikováno v:
Water Resources. 44:442-452
New data on under-ice currents in Lake Baikal have been obtained with the use of high-accuracy instruments. The obtained data were used to analyze the time and space variations of under-ice currents, to calculate the coefficients of horizontal turbul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::014fd054efd0ac787a7d0857bd1409bf
https://doi.org/10.1134/s0097807817030186
https://doi.org/10.1134/s0097807817030186
Publikováno v:
Geography and Natural Resources. 37:212-219
We investigated the influence of deep forced temperature convection on aeration of the bottom water layer in the pelagic zone of Baikal. Temperature T (± 0.002°C) and oxygen O2 concentration (± 0.01 mg/L) were measured by using the SBE-25 probe wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1680a4073d1ec73323d4786629a858e7
https://doi.org/10.1134/s1875372816030045
https://doi.org/10.1134/s1875372816030045
Publikováno v:
Doklady Earth Sciences. 442:272-276
Based on shipboard and satellite observations, the characteristics of upwelling in Lake Baikal in the period of direct temperature stratification have been determined for the first time. Coastal upwellings appear annually under the effect of run-down
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2568672c09cab78c4c3d958caa4a9254
https://doi.org/10.1134/s1028334x12020183
https://doi.org/10.1134/s1028334x12020183
Publikováno v:
Doklady Earth Sciences. 438:652-655
The patterns of renewal of bottom waters in Lake Baikal under the influence of deep convection and intrusion of cold waters have been considered based on the data of temperature surveys of Lake Baikal conducted in 1993–2009. The volumes of the cold
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe13f38f02db7b5885d94024e9e6b003
https://doi.org/10.1134/s1028334x11050096
https://doi.org/10.1134/s1028334x11050096
Publikováno v:
Water Resources. 38:169-174
The specific features of cold bottom intrusion in Baikal are considered based on the results of observations of 1993–2009. It is shown that the intrusion-related renewal of bottom water takes place not regularly and not simultaneously in different
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f197095cc89db147dbd2b25aeb9819cd
https://doi.org/10.1134/s0097807811010143
https://doi.org/10.1134/s0097807811010143
Publikováno v:
Doklady Earth Sciences. 427:804-808
This paper presents the results on measurements of water temperature in Lake Baikal of 1972–2007. The abnormal warming during this period was accompanied by gradual increase of the upper 300 m layer temperature, but did not affect the water state o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7626ce08c08ca25271e7c575fa88fdf
https://doi.org/10.1134/s1028334x09050213
https://doi.org/10.1134/s1028334x09050213
Publikováno v:
Doklady Earth Sciences. 408:645-648
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c3821989d3aca682439ea3022355cbb
https://doi.org/10.1134/s1028334x06040301
https://doi.org/10.1134/s1028334x06040301