DEEP-WATER RENEWAL IN LAKE BAIKAL

dc.contributor.author	Kodenev G.G.
dc.date.accessioned	2021-03-23T04:29:02Z
dc.date.available	2021-03-23T04:29:02Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=14996820
dc.identifier.citation	Russian Geology and Geophysics, 2001, 42, 7, 1127-1136
dc.identifier.issn	1068-7971
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/27040
dc.description.abstract	The paper presents an attempt to describe water exchange in Lake Baikal proceeding from interpretation of tracer (freon-12) contents and temperature of water. Destruction of the metastable equilibrium of the surface water layer in the cold season at reverse stratification is suggested as a controlling mechanism of deep-water renewal. A system of one-dimensional equations of substance (for the tracer) and heat budget is proposed. The solution to an inverse problem for turbulence coefficients and water exchange flows shows a considerable role of turbulence .in the upper layers of deep-water column. The depth-dependent distribution function of sinking surface water parcels is found.
dc.title	DEEP-WATER RENEWAL IN LAKE BAIKAL
dc.type	Статья

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