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- W2388396976 abstract "To investigate the mesoscale characteristics and trigger mechanism of one warm-zone torrential precipitation(WZTP) over complex terrain from 16 to 18 August 2012, conventional observation data, precipitation data of automatic weather stations, TBB data of FY-2E and NCEP 1°×1° reanalysis data are synthesized and analyzed. The results show that the WZTP occurred in the transitional zone between East-ern slope of Tibet Plateau and Sichuan Basin, and was distributed zonally as a belt. Maximum hourly precipitation was located at the area where TBB gradient of MCS was increased. The circulation associated with the WZTP are mainly attributed by the typhoon westward move-ment in the South China Sea and the steady state of Subtropical High. The Subtropical High and warm low-pressure near the surface pre-vented the westerlies trough and cold air from moving across the Longmen Mountain. As a result, the unstable stratification with high energy and temperature over precipitation region can be maintained for a longtime. Furthermore, the convergence of the cold and warm air advec-tions over Longmen Mountain increased the instability of stratification. Finally, the torrential precipitation was triggered by the orography dy-namic lifted by Longmen Mountain." @default.
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- W2388396976 date "2015-01-01" @default.
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- W2388396976 title "Analysis of the characteristics and trigger mechanism of the warm-sector heavy precipitation over complex terrain" @default.
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