Study on Regional Flow Duration Curve and its Uncertaninty
碩士 === 國立交通大學 === 土木工程系 === 87 === Although it has simple theoretical basis, the flow duration curve (FDC) is important in many practical engineering applications. Because of the inherent natural randomness of stream flows, traditional end-of-period FDCs show variation when the selected record lengt...
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ndltd-TW-087NCTU00150242016-07-11T04:13:34Z http://ndltd.ncl.edu.tw/handle/29409486139441483157 Study on Regional Flow Duration Curve and its Uncertaninty 區域化流量延時曲線及其不確定性研究 Shu-yi Wu 吳書易 碩士 國立交通大學 土木工程系 87 Although it has simple theoretical basis, the flow duration curve (FDC) is important in many practical engineering applications. Because of the inherent natural randomness of stream flows, traditional end-of-period FDCs show variation when the selected record lengths are different. It is used to produce a multi-year curve in tradition; however, it is to product annual flow duration curve in this work. In other words, the n-yr-FDC curve is substituted by n annual FDC curves to discuss the statistical characteristics and to divide ally homegeneous hydrologic areas by the cluster analysis. In hydrologic engineering practice, one usually faces the problem of lacking flow discharge data or short record period. Hence, the FDC at the location of interest cannot be derived. Under such circumstances, the regional hydrologic analysis then becomes the commonly adopted methodology. In general, regression analysis is the most common used approach in the regional analysis. In this study, the regional FDCs in each homegenous hydrologic area are derived with their characteristics spcified by the averaged dimensionless form of the FDCs. Furthermone, the ARIMA(Autoregressive Integated Moving Average) model is adopted to estimate future FDCs of the Ho-Long Creek basin. Keh-Chia Yeh 葉克家 1999 學位論文 ; thesis 148 zh-TW |
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碩士 === 國立交通大學 === 土木工程系 === 87 === Although it has simple theoretical basis, the flow duration curve (FDC) is important in many practical engineering applications. Because of the inherent natural randomness of stream flows, traditional end-of-period FDCs show variation when the selected record lengths are different. It is used to produce a multi-year curve in tradition; however, it is to product annual flow duration curve in this work. In other words, the n-yr-FDC curve is substituted by n annual FDC curves to discuss the statistical characteristics and to divide ally homegeneous hydrologic areas by the cluster analysis. In hydrologic engineering practice, one usually faces the problem of lacking flow discharge data or short record period. Hence, the FDC at the location of interest cannot be derived. Under such circumstances, the regional hydrologic analysis then becomes the commonly adopted methodology. In general, regression analysis is the most common used approach in the regional analysis. In this study, the regional FDCs in each homegenous hydrologic area are derived with their characteristics spcified by the averaged dimensionless form of the FDCs. Furthermone, the ARIMA(Autoregressive Integated Moving Average) model is adopted to estimate future FDCs of the Ho-Long Creek basin.
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author2 |
Keh-Chia Yeh |
author_facet |
Keh-Chia Yeh Shu-yi Wu 吳書易 |
author |
Shu-yi Wu 吳書易 |
spellingShingle |
Shu-yi Wu 吳書易 Study on Regional Flow Duration Curve and its Uncertaninty |
author_sort |
Shu-yi Wu |
title |
Study on Regional Flow Duration Curve and its Uncertaninty |
title_short |
Study on Regional Flow Duration Curve and its Uncertaninty |
title_full |
Study on Regional Flow Duration Curve and its Uncertaninty |
title_fullStr |
Study on Regional Flow Duration Curve and its Uncertaninty |
title_full_unstemmed |
Study on Regional Flow Duration Curve and its Uncertaninty |
title_sort |
study on regional flow duration curve and its uncertaninty |
publishDate |
1999 |
url |
http://ndltd.ncl.edu.tw/handle/29409486139441483157 |
work_keys_str_mv |
AT shuyiwu studyonregionalflowdurationcurveanditsuncertaninty AT wúshūyì studyonregionalflowdurationcurveanditsuncertaninty AT shuyiwu qūyùhuàliúliàngyánshíqūxiànjíqíbùquèdìngxìngyánjiū AT wúshūyì qūyùhuàliúliàngyánshíqūxiànjíqíbùquèdìngxìngyánjiū |
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