The structure of precipitation fronts for finite relaxation time

Samuel N. Stechmann, Andrew J. Majda

Research output: Contribution to journalArticle

Abstract

When convection is parameterized in an atmospheric circulation model, what types of waves are supported by the parameterization? Several studies have addressed this question by finding the linear waves of simplified tropical climate models with convective parameterizations. In this paper's simplified tropical climate model, convection is parameterized by a nonlinear precipitation term, and the nonlinearity gives rise to precipitation front solutions. Precipitation fronts are solutions where the spatial domain is divided into two regions, and the precipitation (and other model variables) changes abruptly at the boundary of the two regions. In one region the water vapor is below saturation and there is no precipitation, and in the other region the water vapor is above saturation level and precipitation is nonzero. The boundary between the two regions is a free boundary that moves at a constant speed. It is shown that only certain front speeds are allowed. The three types of fronts that exist for this model are drying fronts, slow moistening fronts, and fast moistening fronts. Both types of moistening fronts violate Lax's stability criterion, but they are robustly realizable in numerical experiments that use finite relaxation times. Remarkably, here it is shown that all three types of fronts are robustly realizable analytically for finite relaxation time. All three types of fronts may be physically unreasonable if the front spans an unrealistically large physical distance; this depends on various model parameters, which are investigated below. From the viewpoint of applied mathematics, these model equations exhibit novel phenomena as well as features in common with the established applied mathematical theories of relaxation limits for conservation laws and waves in reacting gas flows.

Original languageEnglish (US)
Pages (from-to)377-404
Number of pages28
JournalTheoretical and Computational Fluid Dynamics
Volume20
Issue number5-6
DOIs
StatePublished - Nov 2006

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Relaxation Time
Relaxation time
relaxation time
Wetting
Climate models
Steam
Parameterization
Water vapor
Climate Models
Stability criteria
Water Vapor
climate models
parameterization
Flow of gases
Conservation
Drying
Convection
water vapor
Saturation
climate modeling

Keywords

  • Hyperbolic free boundary problems
  • Moisture
  • Nonlinear relaxation equations
  • Tropical atmospheric dynamics
  • Tropical convection

ASJC Scopus subject areas

  • Fluid Flow and Transfer Processes
  • Oceanography
  • Computational Mechanics
  • Mechanics of Materials
  • Applied Mathematics
  • Physics and Astronomy(all)
  • Physics and Astronomy (miscellaneous)
  • Condensed Matter Physics

Cite this

The structure of precipitation fronts for finite relaxation time. / Stechmann, Samuel N.; Majda, Andrew J.

In: Theoretical and Computational Fluid Dynamics, Vol. 20, No. 5-6, 11.2006, p. 377-404.

Research output: Contribution to journalArticle

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