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- W2141093052 abstract "The behavior of the interface between the precipitating and non-precipitating regions is analyzed in an idealized model for the large scale atmospheric circulation. This model uses a quasi-equilibrium relaxation closure in which convection acts to removed the convective instability. It is shown that in the strict quasiequilibrium limit, i.e. for instantaneous convective adjustment, the boundary between the dry and moist regions can exhibit a discontinuity in the precipitation rate and vertical velocity. This interface, referred here to as a precipitation front, behaves as a propagating shock. Three distinct precipitation fronts can be obtained: drying front, slow moistening front and fast moistening front. The front velocity is distinct from the propagation speed of dry and moist disturbances and must be determined by solving a Riemman problem. Stationary precipitation fronts are also found in steady solutions for idealized Walker circulations in both one and two dimensions. Dry gravity waves and coupled convective-gravity waves are partially" @default.
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- W2141093052 date "2007-01-01" @default.
- W2141093052 modified "2023-09-27" @default.
- W2141093052 title "Propagation, reflection and transmission of precipitation fronts in the tropical atmosphere." @default.
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