| 9711号台风移动路径和青岛暴雨的初步分析 |
| |
| 引用本文： | 吴结晶,刘珍芳,韩春深,高留喜.9711号台风移动路径和青岛暴雨的初步分析[J].海洋科学进展,2000,18(1):13-18. |
| |
| 作者姓名： | 吴结晶 刘珍芳 韩春深 高留喜 |
| |
| 作者单位： | 1. 青岛市气象局,青岛,266003
2. 山东省气象台,济南,250031 |
| |
| 摘 要： | 9711号台风受大型环流调整的影响于1997年8月19日14时突然转向北上;20日08～14时该台风北偏东跳跃式移动,是因低空急流使台风倒槽区气旋性环流加强产生新中心所致;青岛地区产生大暴雨则是充沛的水汽、强烈的辐合上升运动与冷空气共同作用的结果.
|
| 关 键 词： | 跳跃式移动 低空急流 台风暴雨 |
| 修稿时间： | 1998-05-29 |
Primary Analysis of the Track of Typhoon 9711 and Storm Rainfall in Qingdao |
| |
| WU Jiejing,LIU Zhenfang,HAN Chunshen,GAO Liuxi.Primary Analysis of the Track of Typhoon 9711 and Storm Rainfall in Qingdao[J].Advances in Marine Science,2000,18(1):13-18. |
| |
| Authors: | WU Jiejing LIU Zhenfang HAN Chunshen GAO Liuxi |
| |
| Abstract: | Due to the
change of circulation pattern, the track of typhoon 9711 turned up northward abruptly at
1400 on Aug. 19, 1997. From 0800 to 1400 on Aug.20 the typhoon jumped northeast,because
the low-level jet enhanced the cyclonic circulation in the region of the trough of
typhoon,and a new cyclonic center appeared. Storm rainfall in Qindao is the result of
cooperation of plenty of water vapor, strong convergence and updraft, and cold air. |
| |
| Keywords: | Jump Low level jet Typhoon and storm |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
