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Numerical experiments on the effects of a meridional ridge on the transmission of energy by barotropic Rossby waves

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Title Numerical experiments on the effects of a meridional ridge on the transmission of energy by barotropic Rossby waves
Names Matano, Ricardo P. (creator)
Date Issued 1995-09-15 (iso8601)
Note copyrighted by American Geophysical Union
Abstract Analytical and numerical models are used to study the effects of
a meridional ridge on the propagation of barotropic Rossby waves produced by
distant wind stress forcing. The analytical model illustrates the qualitative aspects
of the problem by solving a simplified form of the potential vorticity equation. The
analytical results are complemented by numerical experiments using a shallow-water
model. In these experiments, waves are excited near the eastern boundary of the
model. The effect that the presence of a meridional ridge has on the propagation of
these waves is evaluated using spectral analysis. The numerical experiments show
that the ridge acts as a low-pass filter for westward propagating waves. In a 4000-rn
deep ocean a ridge 500 km wide and 500 m high has little effect in preventing energy
transmission by barotropic waves. The topographic effect increases sharply with
the ridge's height so that a 2000-rn ridge almost isolates two neighboring subbasins.
The numerical results indicate that for the range of geophysically relevant cases the
ridge's width plays only a minor role.
Genre Article
Identifier Matano, R.P., Numerical experiments on the effects of a meridional ridge on the transmission of energy by barotropic Rossby waves, J. Geophys. Res.,100, C9.

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