A Tropical Atmosphere Model with Moisture: Global Well-posedness and Relaxation Limit
Jinkai Li, Edriss S. Titi

TL;DR
This paper proves the global well-posedness of a tropical atmosphere model with moisture, and demonstrates its convergence to a limiting system as the relaxation parameter approaches zero, solving an open problem in the field.
Contribution
It establishes the global existence, uniqueness, and continuous dependence of solutions for a moisture-including tropical atmosphere model, and proves its convergence to a limiting system as the relaxation parameter tends to zero.
Findings
Global existence and uniqueness of strong solutions for the model.
Convergence of the system to a limiting system as relaxation parameter tends to zero.
Solution dependence on initial data with additional regularity.
Abstract
In this paper, we consider a nonlinear interaction system between the barotropic mode and the first baroclinic mode of the tropical atmosphere with moisture; that was derived in [Frierson, D.M.W.; Majda, A.J.; Pauluis, O.M.: Dynamics of precipitation fronts in the tropical atmosphere: a novel relaxation limit, Commum. Math. Sci., 2 (2004), 591-626.] We establish the global existence and uniqueness of strong solutions to this system, with initial data in , for each fixed convective adjustment relaxation time parameter . Moreover, if the initial data enjoy slightly more regularity than , then the unique strong solution depends continuously on the initial data. Furthermore, by establishing several appropriate -independent estimates, we prove that the system converges to a limiting system, as the relaxation time parameter tends to zero,…
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