摘要
本文通过对 5月 12日发生在本市的强对流天气分析 ,揭示了 5 .12强对流天气发生的特点和形成机制 ,并初步提出了受华北低涡影响时造成天气显著差异的原因和条件。
The article,through an analysis on strong convection shaped at this locality on May 12th,2000,indicates the shaping mechanism and characteristics of 5.12 strong convection,and preliminarily shows the reasons and conditions of shaping the obvious weather difference affected by low eddies from North China.Thus,it provides us some important clues,aids in forecasting this kind of weather before long.
出处
《气象科学》
CSCD
北大核心
2002年第1期107-112,共6页
Journal of the Meteorological Sciences
