Global well-posedness for passively transported nonlinear moisture dynamics with phase changes. (11th September 2017)

• Record Type: Journal Article
• Authors: Hittmeir, Sabine; Klein, Rupert; Li, Jinkai; Titi, Edriss S
• Is Part Of: Nonlinearity. Volume 30:Number 10(2017:Oct.)
• Page Start: 3676
• Page End: 3718
• Publication Date: 2017-09-11
• Subjects: well-posedness for transport nonlinear moisture dynamics -- moisture model for warm clouds with phase transition -- global existence and uniqueness for a nonlinear moisture model; 35A01 -- 35B45 -- 35D35 -- 35M86 -- 35Q30 -- 35Q35 -- 35Q86 -- 76D03 -- 76D09 -- 86A10; Nonlinear theories -- Periodicals; Mathematical analysis -- Periodicals; Mathematical analysis; Nonlinear theories; Periodicals; 515
• DOI: 10.1088/1361-6544/aa82f1
• Languages: English
• ISSNs: 0951-7715

Abstract

Abstract: We study a moisture model for warm clouds that has been used by Klein and Majda (2006 Theor. Comput. Fluid Dyn .20 525–551) as a basis for multiscale asymptotic expansions for deep convective phenomena. These moisture balance equations correspond to a bulk microphysics closure in the spirit of Kessler (1969 Meteorol. Monogr .10 1–84) and Grabowski and Smolarkiewicz (1996 Mon. Weather Rev .124 487–97), in which water is present in the gaseous state as water vapor and in the liquid phase as cloud water and rain water. It thereby contains closures for the phase changes condensation and evaporation, as well as the processes of autoconversion of cloud water into rainwater and the collection of cloud water by the falling rain droplets. Phase changes are associated with enormous amounts of latent heat and therefore provide a strong coupling to the thermodynamic equation. In this work we assume the velocity field to be given and prove rigorously the global existence and uniqueness of uniformly bounded solutions of the moisture model with viscosity, diffusion and heat conduction. To guarantee local well-posedness we first need to establish local existence results for linear parabolic equations, subject to the Robin boundary conditions on the cylindric type of domains under consideration. We then derive a priori estimates, for proving the maximum principle, using the Stampacchia method, as well as the iterative method by Alikakos (1979 J. Differ. Equ .33 201–25) to obtain uniform boundedness. The evaporation term is of power law type, with an exponent in general less or equal to one and therefore making the proof of uniqueness more challenging. However, these difficulties can be circumvented by introducing new unknowns, which satisfy the required cancellation and monotonicity properties in the source terms.