On thermal convection in stratified fluids
作者:
L. Rahm,
G. Walin,
期刊:
Geophysical & Astrophysical Fluid Dynamics
(Taylor Available online 1979)
卷期:
Volume 13,
issue 1
页码: 51-65
ISSN:0309-1929
年代: 1979
DOI:10.1080/03091927908243760
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
The study of the mechanisms controlling the stratification in closed fluid regions is an important branch of geophysical fluid dynamics. Part of this subject can be handled with a simple linear model, consisting of a buoyancy layer at the non-horizontal boundaries of a container and an advective-diffusive interior coupled by volume continuity. The model is valid under the following conditions: firstly, the buoyancy-frequency characterizing the solution must be sufficiently large to give rise to a flow pattern of boundary layer type and, secondly, the non-horizontal walls must not have too large thermal conductivity.
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