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Article information
2007 , Volume 12, ¹ 6, p.59-72
Ovchinnikova T.E., Bocharov O.B.
Seasonal effect of tributary water on water exchange in a deep lake with significant bottom inclination
An effect of mineralized warm tributary on the development of density flows in Lake Baikal during different seasons is investigated by means of numerical experiments using a two-dimensional vertical mathematical model of hydrophysical processes. The region of Kukui Canyon with the bottom slope close to 3*10-2 was selected as an example for calculation. It has been shown that under the conditions of such slope and for various mineralizations of the tributary and the lake, the plunge of the river waters is deepest during the period of spring heating.
[full text] Author(s):
Ovchinnikova Tamara Eduardovna
PhD. , Associate Professor
Position: Senior Research Scientist
Office: Institute for Water and Environmental Problems of the Siberian Branch Russian Academy of Sciences
Address: 656038, Russia, Barnaul, Molodezhnaya str., 1
Phone Office: (383) 330-20-05
E-mail: teonew@iwep.nsc.ru
SPIN-code: 1676-1371Bocharov Oleg Borisovich
PhD. , Associate Professor
Position: Research Scientist
Office: Baker Hughes Incorporation
Address: 630128, Russia, Novosibirsk, Kutateladze 4a
Phone Office: (383) 3329443
E-mail: Oleg.Bocharov@bakerhughes.com
Bibliography link:
Ovchinnikova T.E., Bocharov O.B. Seasonal effect of tributary water on water exchange in a deep lake with significant bottom inclination // Computational technologies. 2007. V. 12. ¹ 6. P. 59-72
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