“海棠”台风风浪场分析  

Characteristic analysis of wind waves induced by Typhoon Haitang (0505)

作　　者：吴晓峰[1] 于芸[1] 邓小东[1] 徐丽丽[1] 

机构地区：[1]国家海洋局东海预报中心,上海200081

出　　处：《海洋预报》2009年第3期86-92,共7页Marine Forecasts

摘　　要：通过对0505号"海棠"台风的高、低空气流场的分析,揭示了"海棠"台风浪成长、发展、消衰的机制和规律。结果表明:台风浪的大小和范围不仅与台风的强度、移速及周围大尺度天气系统有关,而且也受岛屿及海底地形等环境条件的影响。Based on the analysis of the lower and upper air flow fields of Typhoon Haitang （0505）, the mechanism of evolution, development and downgrade of typhoon-induced wind waves was studied in this paper. It was shown that the magnitude and range of wind waves are not only related to the strength, moving speed and the surrounding large-scale meteorological systems of the typhoon, but also influenced bv the island and topography of sea floor.

关 键 词：台风 风区 风时 风浪 涌浪 

分 类 号：P444[天文地球—大气科学及气象学]