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題 名 | 民國八十六年颱風暴潮調查報告--溫妮颱風與安珀颱風=Report on Typhoon Surges of 1997--Typhoon Winnie and Typhoon Amber |
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作 者 | 曾淑芬; 李汴軍; | 書刊名 | 氣象學報 |
卷 期 | 43:1 1999.12[民88.12] |
頁 次 | 頁27-44 |
分類號 | 328.55 |
關鍵詞 | 颱風暴潮; Typhoon-induced storm surge; |
語 文 | 中文(Chinese) |
中文摘要 | 本文之目的是敘述民國86年兩個主要侵襲臺灣的溫妮與安珀颱風,對臺灣沿岸所 產生的暴潮現象。溫妮颱風中心經過臺灣北部海面,由於其結構很好,而且颱風範圍甚大, 當颱風環流直接吹向臺灣北部沿岸時,加上氣壓下降導致明顯之暴潮,期間以新竹潮位站所 量測到暴潮 2.6 公尺為最大。 安珀颱風是在花蓮秀姑巒溪北邊登陸,在整個颱風影響臺灣 期間,西部雲林、嘉義沿岸暴潮比東海岸還要明顯,其他海岸暴潮現象則與颱風接近臺灣遠 近有關。當颱風登陸後,環流被破壞,各地暴潮現象大部分比較小。 |
英文摘要 | The aim of this paper is to describe the storm surge phenomena, induced by the two enajor typhoons WINNIE and AMBER in 1997. When typhoon WINNIE passed over the northern Taiwan waters, its structures were well defined and its influencing area was large. The circulation of WINNIE caused big storm surges directly toward the northern coast of Taiwan and dropped the pressure down deeply. The maximum surge up to 2.6 m was measured at Hsinchu tidal station. Whereas typhoon AMBER made landfall at the northern part of the Shiowguluan creek. During the influencing time of typhoon AMBER, the storm surges observed at Yunlin and Chiayi were obviously larger than those at the eastern coast of Taiwan The surges of other coastal area were relevant to the distance between typhoon center and coast. After landfall, AMBER's structure broke very soon, the surges were small over the coast island-wide. |
本系統中英文摘要資訊取自各篇刊載內容。