Deep-water renewal in Lake Baikal

被引:0
|
作者
Kodenev, GG [1 ]
机构
[1] Russian Acad Sci, Geophys & Ecol Tool Making Design Technol Inst, Novosibirsk 630090, Russia
来源
GEOLOGIYA I GEOFIZIKA | 2001年 / 42卷 / 07期
关键词
chemical tracers; renewal time; heat and mass exchange;
D O I
暂无
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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.
引用
收藏
页码:1127 / 1136
页数:10
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