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Analysis of Barotropic Model

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Mathematics of Climate Modeling

Abstract

In this chapter we shall consider the following equations of the barotropic atmosphere on rotating sphere S2R3 with radius a:

$$\frac{\partial }{{\partial t}}\Delta \psi + J\left( {\psi ,\Delta \psi + l} \right) = - \sigma \Delta \psi + v\mathop \Delta \nolimits^2 \psi + f,\quad \psi \left| {_{t = 0} } \right.\; = \;\psi _0 ,$$
(3.1)

and

$$\frac{\partial }{{\partial t}}\Delta \psi + J\left( {\psi ,\Delta \psi + l} \right) = - \sigma \Delta \psi + v\mathop {\left( { - \Delta \,} \right)}\nolimits^{s + 1} \psi + f,\quad \psi \left| {_{t = 0} } \right.\; = \;\psi _0 ,$$
(3.2)

where ψ is the stream-function, J(a,b) is the Jacobian, l = 2Ω sin φ, s ≥ 1, while the parameters Ω > 0 and σ ≥ 0 have the dimensions [Ω] = T−1, [σ] = T−1, respectively.

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© 1997 Birkhäuser Boston

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Dymnikov, V.P., Filatov, A.N. (1997). Analysis of Barotropic Model. In: Mathematics of Climate Modeling. Modeling and Simulation in Science, Engineering, & Technology. Birkhäuser Boston. https://doi.org/10.1007/978-1-4612-4148-5_3

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  • DOI: https://doi.org/10.1007/978-1-4612-4148-5_3

  • Publisher Name: Birkhäuser Boston

  • Print ISBN: 978-1-4612-8674-5

  • Online ISBN: 978-1-4612-4148-5

  • eBook Packages: Springer Book Archive

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