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.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.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.title | DEEP-WATER RENEWAL IN LAKE BAIKAL | |
| dc.type | Статья |