The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition

碩士 === 國立屏東科技大學 === 土木工程系所 === 101 === Reliable estimations of missing data is an important task for hydrologists, engineers and environmental researchers. This study applies the correlation analysis to assess the accuracy of the rainfall station network for Yenshui river basin. In addition, employ...

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Main Authors: Shiang-Min Chen, 陳香旻
Other Authors: Yu-Min Wang
Format: Others
Language:zh-TW
Published: 2012
Online Access:http://ndltd.ncl.edu.tw/handle/68312329588452551811
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spelling ndltd-TW-101NPUS50150102016-12-22T04:18:36Z http://ndltd.ncl.edu.tw/handle/68312329588452551811 The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition 集水區現有測站缺測下之平均雨量修正與推估 Shiang-Min Chen 陳香旻 碩士 國立屏東科技大學 土木工程系所 101 Reliable estimations of missing data is an important task for hydrologists, engineers and environmental researchers. This study applies the correlation analysis to assess the accuracy of the rainfall station network for Yenshui river basin. In addition, employ Thiessen polygons to compare maximum one-day precipitation variations in the basin. The objective is to study the effects on watershed rainfall estimation in case data is missing in one of the stations in the network. Then, we apply frequency analysis for comparing maximum one-day rainfall in different return periods. From the correlation analysis, relationship among the stations is high having correlation between 0.75 and 0.96. Thiessen polygons method shows that in Heshun rainfall station (P04) the weight is highest and in Qiding rainfall station (P05) is lowest. For frequency analysis based on the results, we suggest using the Log Pearson type III method to estimate the return periods of 25, 50, 100 and 200 year in Yenshui River. When P04 is omitted in a 25 year return period the maximum one-day precipitation is 484 mm, Hutoupi rainfall station (P01) is 463 mm and Xinshi rainfall station (P07) is 445mm. In this study it revealed that using Thiessen polygons analysis alone is insufficient and unreliable. Instead, more than one form of analysis should be taken into account in the adjustment and estimation of watershed rainfall under missing records condition. Yu-Min Wang 王裕民 2012 學位論文 ; thesis 52 zh-TW
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language zh-TW
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sources NDLTD
description 碩士 === 國立屏東科技大學 === 土木工程系所 === 101 === Reliable estimations of missing data is an important task for hydrologists, engineers and environmental researchers. This study applies the correlation analysis to assess the accuracy of the rainfall station network for Yenshui river basin. In addition, employ Thiessen polygons to compare maximum one-day precipitation variations in the basin. The objective is to study the effects on watershed rainfall estimation in case data is missing in one of the stations in the network. Then, we apply frequency analysis for comparing maximum one-day rainfall in different return periods. From the correlation analysis, relationship among the stations is high having correlation between 0.75 and 0.96. Thiessen polygons method shows that in Heshun rainfall station (P04) the weight is highest and in Qiding rainfall station (P05) is lowest. For frequency analysis based on the results, we suggest using the Log Pearson type III method to estimate the return periods of 25, 50, 100 and 200 year in Yenshui River. When P04 is omitted in a 25 year return period the maximum one-day precipitation is 484 mm, Hutoupi rainfall station (P01) is 463 mm and Xinshi rainfall station (P07) is 445mm. In this study it revealed that using Thiessen polygons analysis alone is insufficient and unreliable. Instead, more than one form of analysis should be taken into account in the adjustment and estimation of watershed rainfall under missing records condition.
author2 Yu-Min Wang
author_facet Yu-Min Wang
Shiang-Min Chen
陳香旻
author Shiang-Min Chen
陳香旻
spellingShingle Shiang-Min Chen
陳香旻
The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
author_sort Shiang-Min Chen
title The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
title_short The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
title_full The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
title_fullStr The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
title_full_unstemmed The Correction and Estimation of Watershed Average Rainfall under Missing Records Condition
title_sort correction and estimation of watershed average rainfall under missing records condition
publishDate 2012
url http://ndltd.ncl.edu.tw/handle/68312329588452551811
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