A simple model for unsteady buoyancy-driven abyssal circulation
作者:
AndrewJ. Willmott,
RogerH. J. Grimshaw,
期刊:
Geophysical & Astrophysical Fluid Dynamics
(Taylor Available online 1995)
卷期:
Volume 81,
issue 3-4
页码: 131-158
ISSN:0309-1929
年代: 1995
DOI:10.1080/03091929508229061
出版商: Taylor & Francis Group
关键词: Abyssal plain;quasigeostrophic;stratification.
数据来源: Taylor
摘要:
This paper considers oceanic buoyancy driven flow using the linearised equations for a continuously stratified, incompressible, inviscid, Boussinesq fluid. The ocean is unbounded horizontally, infinitely deep and has a linear sloping bottom of arbitrary orientation. Initially the fluid is at rest with uniform buoyancy frequency. Then a point mass source, located on the sea floor, is switched-on and maintained. Using quasigeostrophic theory, explicit analytical solutions are found for the case of (a) a mid-latitude β-plane when the bottom is flat, or (b) anf-plane in the presence of a sloping bottom. In the former case the solutions complement those obtained by McDonald (1992) while in the latter case a two-dimensional bottom trapped wave response is generated.
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