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國家級防災監測及模式測試基地 - 說明

台灣位於歐亞大陸與太平洋交界之季風區,雖然台灣年平均雨量可達2,500公釐,但降雨之時空分佈卻極不均勻,山區之年平均降雨量有時高達5,000公釐,但部分平地地區卻僅有1,000公釐,加上台灣集水區上游坡度陡峭,河短流急,每逢颱風或豪雨來襲,山區匯集而下之洪流,易造成河川水位暴漲,再加上近年來受到降雨強度增加與都市化效應的影響,使得地表逕流量增加和集水區集流時間縮短,若碰上排水系統宣洩不及,則易造成淹水,對人民生命財產產生莫大的威脅。

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國家級防災監測及模式測試基地 - 說明 | wraew.ttfri.narlabs.org.tw Reviews
<META>
DESCRIPTION
台灣位於歐亞大陸與太平洋交界之季風區,雖然台灣年平均雨量可達2,500公釐,但降雨之時空分佈卻極不均勻,山區之年平均降雨量有時高達5,000公釐,但部分平地地區卻僅有1,000公釐,加上台灣集水區上游坡度陡峭,河短流急,每逢颱風或豪雨來襲,山區匯集而下之洪流,易造成河川水位暴漲,再加上近年來受到降雨強度增加與都市化效應的影響,使得地表逕流量增加和集水區集流時間縮短,若碰上排水系統宣洩不及,則易造成淹水,對人民生命財產產生莫大的威脅。
<META>
KEYWORDS
1 計畫簡介
2 宜蘭河流域
3 典寶溪流域
4 資料下載
5 相關連結
6 鑒此,以 宜蘭河
7 與 典寶溪排水
8 委託單位 經濟部水利署水利規劃試驗所
9 執行單位 台灣颱風洪水研究中心
10 淡江大學水資源管理與政策研究中心
CONTENT
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PAGE
計畫簡介,宜蘭河流域,典寶溪流域,資料下載,相關連結,鑒此,以 宜蘭河,與 典寶溪排水,委託單位 經濟部水利署水利規劃試驗所,執行單位 台灣颱風洪水研究中心,淡江大學水資源管理與政策研究中心,成功大學水工試驗所,台灣大學水工試驗所,財團法人國家實驗研究院台灣颱風洪水研究中心 2012
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國家級防災監測及模式測試基地 - 說明 | wraew.ttfri.narlabs.org.tw Reviews

https://wraew.ttfri.narlabs.org.tw

台灣位於歐亞大陸與太平洋交界之季風區,雖然台灣年平均雨量可達2,500公釐,但降雨之時空分佈卻極不均勻,山區之年平均降雨量有時高達5,000公釐,但部分平地地區卻僅有1,000公釐,加上台灣集水區上游坡度陡峭,河短流急,每逢颱風或豪雨來襲,山區匯集而下之洪流,易造成河川水位暴漲,再加上近年來受到降雨強度增加與都市化效應的影響,使得地表逕流量增加和集水區集流時間縮短,若碰上排水系統宣洩不及,則易造成淹水,對人民生命財產產生莫大的威脅。

INTERNAL PAGES

wraew.ttfri.narlabs.org.tw wraew.ttfri.narlabs.org.tw
1

宜蘭河流域

http://wraew.ttfri.narlabs.org.tw/yilanr.php

2

相關連結

http://wraew.ttfri.narlabs.org.tw/link.php

Monitoring and Research Activities in the Goodwin Creek Experimental Watershed. Walnut Gulch Experimental Watershed.

3

國家級防災監測及模式測試基地 - 說明

http://wraew.ttfri.narlabs.org.tw/index.php

台灣位於歐亞大陸與太平洋交界之季風區,雖然台灣年平均雨量可達2,500公釐,但降雨之時空分佈卻極不均勻,山區之年平均降雨量有時高達5,000公釐,但部分平地地區卻僅有1,000公釐,加上台灣集水區上游坡度陡峭,河短流急,每逢颱風或豪雨來襲,山區匯集而下之洪流,易造成河川水位暴漲,再加上近年來受到降雨強度增加與都市化效應的影響,使得地表逕流量增加和集水區集流時間縮短,若碰上排水系統宣洩不及,則易造成淹水,對人民生命財產產生莫大的威脅。

4

資料下載

http://wraew.ttfri.narlabs.org.tw/data.php

5

典寶溪流域

http://wraew.ttfri.narlabs.org.tw/dbc.php

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