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《Plateau Meteorology》 2000-04
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THREE-PHASE CLOUD EXPLICITY PRECIPITATION SCHEME AND MESOSCALE NUMERICAL SIMULATION FOR GENERATED CAUSE OF THE “96.1” SNOWSTORM

DENG Yuan ping CHENG Lin sheng ZHANG Xiao ling (Department of Atmospheric Sciences, Lanzhou University, Lanzhou, Gansu 730000)  
The analysis of generated cause for the “96.1” snowstorm event over Qinghai Xizang Plateau was conducted using weather observational data. The results indicated that the European blocking high collapsed, the cold trough transformed from transversal into upright, the southwards invading cold and dry air flow behind the trough and the northwards intensive southwest warm wet air flow coming from the Bay of Bengal and the Indian peninsula were converged over northeastern part of Qinghai Xizang Plateau while a mesoscale shear line was formed and persistent developed. This shear line was main mesoscale weather system of producing the “96.1” snowstorm over Qinghai Xizang Plateau. A mesoscale model and simulation system was developed through incorperating an ice phase cloud microphysics process parameterization and a three phase cloud explicity precipitation scheme. The genesis and development as well as evolutive structure of a mesoscale shear line associated with the “96.1” snowstorm over Qinghai Xizang Plateau were basically successful simulated under the condition of using conventional observational data. The results showed that the developed and improved mesoscale model and simulation system is suitable for numerical simulation research of the genesis, development and structural evolution of mesoscale system over Qinghai Xizang Plateau of possessing complex topography and underlying surface. Space time evolution of simulated streamline field and physical fields revealed that the space time evolutive consistence of the convergence line of the streamline field with the shear line associated snowstorm showed the expression of the mesoscale system over Qinghai Xizang Plateau that is essential important by using streamline field possesses. An important mechanism of the genesis and development for the snowstorm shear line was that the divergence on upper levels was more intensive than convergence on lower levels and a dynamic coupling of positive vorticity zone with convergent zone. The intension and persistence of vertical ascending motion was a necessary condition of vapor condensation and snow formed by freezing. The deep, thick, wet tongue and moist convection instability supplied abundant moisture source and thermal instability condition. The superposition of the deep, thick, wet tongue and the convergent zone as well as the ascending motion was an intensive coupling structure for the formation and persistence of the snowstorm. The roughly consistence between the snowstorm zone and precipitation with that of the observational analysis showed the three phase cloud explicity precipitation scheme is basical reasonable.
【Fund】: 国家自然科学基金!(497752 71 )资助
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