摘要
1995年6月8～9日闽南局部地区大暴雨主要是受南侵的冷空气和9502号热带风暴的共同影响而产生。该冷空气来源于整个西北地区和青藏高原东部，范围较大，由于受云贵高原地形的影响，槽在东移过程中表现出如下特点：大槽发生倾斜、断裂，然后又在沿海地区合并；大精的结构特征为垂直方向同相位；在华南形成中尺度热带云团随西南气流北上影响闽南地区。与此同时，9502号热带风暴穿过台湾海峡与槽前云系相互作用。上述原因形成了厦门地区大暴雨。
The torrential rain occurred in the region of Xiamen from June 8 to 9, 1995 was produced by strong co1d air and troptical storm No. 9502. The large amount of Cold air came from the northwest of China and the east of Qinghai-Tibet Plateau and was subject the topographic effects of Yunnan-Guizhou Plateau on it way moving eastward. There are three characters in this process as follows. 1. As the upper trough moved east, it sloped, fractured and merged in the coastal region of East China. 2. The structure of the upper trough was in the same phase vertically. 3. Mesoscale tropical cloud clusters, which drived from South China, moved northward with the SW jet and exercised effects on the south Fujian. In the same time, tropical storm No. 9502 went through the Taiwan Strait and acted on the cloud system in front of the upper trough. These are the causes for the occurring of trrential rain in Xiamen area.
出处
《台湾海峡》
CAS
CSCD
1997年第1期17-20,共4页
Journal of Oceanography In Taiwan Strait
