| 研究生: |
鐘偉誠 Zhong, Wei-Cheng |
|---|---|
| 論文名稱: |
高屏溪未量測集水區流量歷線推估之研究 A Study on the Estimation of Hydrograph in Ungauged Catchments of Kao-Ping River |
| 指導教授: |
游保杉
Yu, Pao-Shan |
| 學位類別: |
碩士 Master |
| 系所名稱: |
工學院 - 水利及海洋工程學系 Department of Hydraulic & Ocean Engineering |
| 論文出版年: | 2004 |
| 畢業學年度: | 92 |
| 語文別: | 中文 |
| 論文頁數: | 83 |
| 中文關鍵詞: | 分布型降雨-逕流模式 、無因次單位歷線 、區域分析 、未量測集水區 |
| 外文關鍵詞: | Distributed Rainfall-Runoff Model, Dimensionless Unit Hydrograph, Regional Analysis, Ungauged Catchment |
| 相關次數: | 點閱:135 下載:11 |
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未量測集水區(ungauged catchments)為近年來水文模式研究與應用之重點。而台灣以往估算未量測集水區之流量歷線常使用無因次單位歷線法來模擬。本研究擬提出另一套替代方法,首先乃綜合暴雨事件與流域內集水區特性,針對三個流量歷線重要特性參數(即尖峰流量、尖峰發生時刻與總逕流體積)建立區域關係。本研究以高屏溪流域為研究區域,將其內八個子集水區挑選出26場暴雨事件進行流量歷線重要特性參數之區域分析。主要利用雨量及雨型之重要參數並且搭配數值高程模式(DTM)與地理資訊系統(GIS)軟體所建立之地文因子,建構三個流量歷線重要參數之區域公式。於驗證過程中,採用交叉輪流驗證方法,發現可合理模擬未量測集水區之流量歷線重要參數。進一步利用此三目標函數值配合分布型降雨-逕流模式,使用模糊多目標函數率定方法完成模式參數之率定,以推求未量測集水區完整之流量歷線,比傳統無因次單位歷線法有較好之模擬結果。
Recently, many researches have paid much attention on hydrological model in ungauged catchments. In the past, method of dimensionless unit hydrograph is often used on hydrological prediction in ungauged catchments of Taiwan. The study aims to provide other substitute method. First, to develop the regional relationships for three important characteristics of hydrograph, i.e. time to peak, peak flow, and total runoff volume respectively, using the characteristics of storm event and catchment. Twenty-six storm events from eight sub-catchments in Kao-Ping River basin provided the analysis data in the study area. The characteristics and physiographic factors of studied catchments, which are generated using both DTM and GIS software, are used to develop the regional formula for these three important hydrograph parameters. The cross validation results reveal that the method proposed in this work can reasonably simulate the parameters of hydrograph at ungauged catchments. Then, the three important hydrograph parameters were further applied to the distributed rainfall-runoff model calibration with fuzzy multi-objective function. Finally, the hydrograph of unguaged catchments can be obtained and the result has a better performance on hydrograph simulation than tradition method of dimensionless unit hydrograph.
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