Beta plane approximation

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March 30, 2010, 12:00 am
December 10, 2011, 11:46 am

The beta plane approximation, in oceanography and general fluid dynamics, is a simplified coordinate system for the equations of motion where the variation of the Coriolis parameterf with latitude is approximated by

f = f0 + βy

where f0 is the value of f at the mid-latitude of the region and β the latitudinal gradient of f at that same latitude. This formalism is used to investigate both equatorial and mid-latitude phenomena (for which there are slightly different beta plane approximations) where f varies significantly over a few tens of degrees latitude. The beta plane approximation allows considerable simplification of the governing equations and therefore the use of analytical investigation methods. See Gill [1982].

The beta plane equations are obtained by introducing a background stratification into the shallow water equations, expanding them around a reference latitude θ0 with respect to ε~ θ − θ0, and keeping terms up to first order in ". This approximation introduces the horizonal coordinates

x = r0 cos θ0(φ − φ0)
y = r0(θ − θ0)

and expands the Coriolis parameter as

f = f0 + β0y + • • •

where β0 is the beta paramter at the reference latitude. The resulting equations (after Muller [1995])

are:

Img62.png Image:Img62.png + Img64.png Image:Img64.png - Img66.png Image:Img66.png = Img67.png Image:Img67.png

Img68.png Image:Img68.png + Img69.png Image:Img69.png + Img70.png Image:Img70.png

0 = Img72.png Image:Img72.png

Img73.png Image:Img73.png = Img74.png Image:Img74.png

Img75.png Image:Img75.png + Img76.png Image:Img76.png

where (u, v,w) are the velocity components in the (x, y, z) directions, r0 is the mean radius of the Earth, θ0 is the reference latitude, f0 = 2Ωsin θ0 is the Coriolis parameter at the reference latitude, Img81.png Image:Img81.png is the beta parameter at the reference latitude, ρ* is a constant reference density, δp and δρ are motionally induced deviations from prescribed background fields, and N is the buoyancy frequency.

This article is written at a definitional level only. Authors wishing to expand this entry are inivited to expand the present treatment, which additions will be peer reviewed prior to publication of any expansion.

Further Reading

  • J.R.Holton. 2004. An introduction to dynamical meteorology, Academic Press. ISBN 978-0123540157.
  • Physical Oceanography Index

Citation

Baum, S. (2011). Beta plane approximation. Retrieved from http://editors.eol.org/eoearth/wiki/Beta_plane_approximation