The fluid dynamic model under investigation stems from the tropical climate model [D. M. W. Frierson, A. J. Majda and O. M. Pauluis, Commun. Math. Sci. 2 (2004), no. 4, 591--626; MR2119930 (2006a:86015)] written, under suitable approximations, for the three observables: baroclinic velocity u⃗ , temperature deviation T, and moisture q, all made dimensionless. The interested reader should also look at the references, [D. M. W. Frierson, A. J. Majda and O. M. Pauluis, op. cit.] in particular, in order to fully appreciate the breadth of this paper.
Crosta, G. (2011). Mathematical Review: MR2681475 (2011h:35170) Majda, Andrew J.; Souganidis, Panagiotis E. Existence and uniqueness of weak solutions for precipitation fronts: a novel hyperbolic free boundary problem in several space variables. MATHEMATICAL REVIEWS.
Mathematical Review: MR2681475 (2011h:35170) Majda, Andrew J.; Souganidis, Panagiotis E. Existence and uniqueness of weak solutions for precipitation fronts: a novel hyperbolic free boundary problem in several space variables.
CROSTA, GIOVANNI FRANCO FILIPPO
2011
Abstract
The fluid dynamic model under investigation stems from the tropical climate model [D. M. W. Frierson, A. J. Majda and O. M. Pauluis, Commun. Math. Sci. 2 (2004), no. 4, 591--626; MR2119930 (2006a:86015)] written, under suitable approximations, for the three observables: baroclinic velocity u⃗ , temperature deviation T, and moisture q, all made dimensionless. The interested reader should also look at the references, [D. M. W. Frierson, A. J. Majda and O. M. Pauluis, op. cit.] in particular, in order to fully appreciate the breadth of this paper.
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