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- W2989043672 abstract "Three-dimensional simulation of cold-front rain-band (NC'FR) associated with a straight cold front has been studied by use of a non-hydrostatic, full compressible storm-scale model (ARPS) including multi-phase microphysical parameterization. The dynamical and physical features of the frontal cloud de-velopment have been well simulated and analyzed. It is in evidence that the frontal cloud is triggered by the updraft of the secondary frontal circulation. However, the long persistence of diabalic fronlogenesis only can be attributed to positive feedback between the frontal baroclinicity and the prefrontal latent heat release. The simulations indeed demonstrate that the potential temperature gradient enhancement in front zone is strongly related wilh the re-distribution of cloud moisture, by the action of tilted updraft. In conse-quence, the splice of cooling and heating pool that is respectively created from the evaporation of cloud wat er and condensing/ freezing of water vapor/ rain droplet, wich is in favor of the strong contrast of cool and warm air mass across the frontal zone to diabatic frontogenesis." @default.
- W2989043672 created "2019-11-22" @default.
- W2989043672 creator A5061563330 @default.
- W2989043672 date "2002-01-01" @default.
- W2989043672 modified "2023-09-23" @default.
- W2989043672 title "Interaction of Diabatic Frontogenesis and MoistureProcesses in Cold-Frontal Rain-Band" @default.
- W2989043672 hasPublicationYear "2002" @default.
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