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52 (1995), 3779–3796. [53] J. Pedlosky, Geophysical Fluid Dynamics. Springer-Verlag, New York, 1979. [54] Yu. N. Skiba, I. Peres-Garcia, On the structure and growth rate of unstable modes to the Rossby-Haurwitz wave. Numerical Methods for Partial Differential Equations 21 (2005), 368–386. ISBN 978-1-60876-265-1 In: Advances in Mathematics Research, Volume 10 c 2010 Nova Science Publishers, Inc. Editor: Albert R. Baswell, pp. 29-52 Chapter 2 ∞−D IMENSIONAL C EREBELLAR C ONTROLLER FOR R EALISTIC H UMAN B IODYNAMICS Vladimir G.

The fibers coming down from cerebral cortex, however, do need to cross (as the cerebrum is concerned with the opposite side of the body, unlike the cerebellum). These fibers synapse in the pons (hence the huge block of fibers in the cerebral peduncles labelled ‘cortico–pontine’), cross, and enter the cerebellum as mossy fibers. The 3 deep nuclei are the fastigial, interposed, and dentate nuclei. The fastigial nucleus is primarily concerned with balance, and sends information mainly to vestibular and reticular nuclei.

Academic Press, New York, 1966. [49] J. La Salle, S. Lefschetz, Stability by Liapunov’s Direct Method. Academic Press, New York (1961). [50] P. Ripa, Positive, negative and zero wave energy and the flow stability problem in the Eulerian and Lagrangian-Eulerian descriptions. Pure and Applied Geophysics 133 (1990), 713–732. 28 Yuri N. Skiba [51] Mankin Mak, Ming Cai, Local barotropic instability. J. Atm. Sci. 46 (1989), 3289– 3311. [52] M. D. Borges, P. D. Sardeshmukh, Barotropic Rossby wave dynamics of zonally varying upper-level flows during northern winter.

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