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Num ericalExperim ent ofTrumpet-shaped Topography Influence on a Heavy Rain
DUAN Hai-Xia, LIU Xin-Wei
J4    2009, 27 (4): 327-333.  
Abstract1576)      PDF(pc) (2840KB)(2629)       Save

Theweather systems and a relatedmesoscal convective systems, causing severe heavy rain in the south-eastGansu Province during 27-28 Aug 2006, are successfully simulatedwithMM5 models. Trumpet-shaped topography prominently increased rainfall in Gangu county. The rise of the terrain enhanced the low level convergence and verticalmovementover thewindward side of the terrain.The dynamical enforced rise of the terrain emerged at the prophase and the time of the rainfal.l

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Application of Surfer Automation Technique in Automatic M apping for M eteorological Data
ZHANG Tie-Jun, WANG Ti-Wen, ZHANG Hong, LIU Xin-Wei
J4    2007, 25 (2): 90-94.  
Abstract939)      PDF(pc) (236KB)(2100)       Save

The main functions of Surfer software,ActiveX automation technique and the interface of VB application and Surfer are introduced in this paper.It is also introduced how to combine the strong ability of development using VB software and the strong mapping in  Surfer based on the interface.and the key program to Ca/Ty out the interface technique and a case of application automatic mapping are presented.

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Analysis of Formation Cause About a Rare Fog in East China
ZHANG Xin-Rong, LIU Chi-Guo, YANG Jian-Cai, LIU Xin-Wei, CHENG Feng
J4    2006, 24 (3): 47-51.  
Abstract1886)      PDF(pc) (445KB)(2873)       Save

The large range rare fog process which occurred in East China from November 30 to December 4 in 2004 was analyzed, including the circulation background, its adjustment and evolvement, the climatic background, the atmospheric stratification condition and the vapor condition near surface, etc. Results show that the warm advection at the low level, the stable atmospheric stratification and the abundant vapor condition resulted in this rare fog process, and fog dissipation needs the cold air invasion with the cold front.

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Analysis of Circulation Characteristic for Abnormal High Temperature over the Northeast Side of Tibetan Plateau
LIU Xin-Wei, DIAO Qiang-Yun, SUN Guo-Wu
J4    2006, 24 (3): 42-46.  
Abstract1835)      PDF(pc) (390KB)(2150)       Save
The summer high temperature trend over the northeast side of the Tibetan Plateau was investigated by using the daily high temperature data (1960-2003) of 80 stations there and 30 years (1971-2000) NCEP/NCAR reanalysis data, and by selecting the typical case of abnormal high temperature, the circulation characteristic and the possible region influenced by the same weather process were analyzed. It was found that if the westerly index varied from high to low and maintained, the high temperature weather would occur and last, on the contrary, it would end. The main circulation characteristic of the high temperature weather was the addition of the South Asia high and the Northwest Pacific subtropical high. The positive temperature advection of the upper level and the negative vorticity throughout the whole level also induced the persistence of the high temperature weather. The temperature change over Lanzhou and its surrounding areas was consistent, when temperature high over Lanzhou, the northeast side of the Tibetan Plateau would reach the high temperature at the same time. 
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