Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan
碩士 === 淡江大學 === 水資源及環境工程學系碩士班 === 98 === The purpose of this study was to introduce a simple method for estimating stream flow with the exceedance probability of 85% (Q85) from readily available mean specific discharge data and catchment area. First of all, for each of the four streaflow stations lo...
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ndltd-TW-098TKU050870062015-10-13T18:20:59Z http://ndltd.ncl.edu.tw/handle/42771180469815464406 Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan 石門水庫上游集水區地面水潛能水量推估之研究 Po-Jui kung 龔柏叡 碩士 淡江大學 水資源及環境工程學系碩士班 98 The purpose of this study was to introduce a simple method for estimating stream flow with the exceedance probability of 85% (Q85) from readily available mean specific discharge data and catchment area. First of all, for each of the four streaflow stations located in Shihmen watershed, the dimensionless Q85 (normalized using monthly? mean stream flow) for each month of the year was estimated from past daily stream flow records. An accurate estimation of Q85 required a minimal time series length of 10 to 20. The dimensionless Q85 for different months of the year were then plotted against the respective specific mean discharges. A best fit curve was then determined based on adjusted R-square values. The correlation between Q85 and specific mean discharge for each station is described ay a unique curve. Once the best-fit curve for a specific stream gage is determined, Q85 for that specific location in the future then can be estimated from its updated specific mean discharge and the catchment area. Gwo-Hsing Yu 虞國興 2010 學位論文 ; thesis 126 zh-TW |
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Others
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碩士 === 淡江大學 === 水資源及環境工程學系碩士班 === 98 === The purpose of this study was to introduce a simple method for estimating stream flow with the exceedance probability of 85% (Q85) from readily available mean specific discharge data and catchment area. First of all, for each of the four streaflow stations located in Shihmen watershed, the dimensionless Q85 (normalized using monthly? mean stream flow) for each month of the year was estimated from past daily stream flow records. An accurate estimation of Q85 required a minimal time series length of 10 to 20. The dimensionless Q85 for different months of the year were then plotted against the respective specific mean discharges. A best fit curve was then determined based on adjusted R-square values. The correlation between Q85 and specific mean discharge for each station is described ay a unique curve. Once the best-fit curve for a specific stream gage is determined, Q85 for that specific location in the future then can be estimated from its updated specific mean discharge and the catchment area.
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author2 |
Gwo-Hsing Yu |
author_facet |
Gwo-Hsing Yu Po-Jui kung 龔柏叡 |
author |
Po-Jui kung 龔柏叡 |
spellingShingle |
Po-Jui kung 龔柏叡 Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
author_sort |
Po-Jui kung |
title |
Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
title_short |
Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
title_full |
Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
title_fullStr |
Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
title_full_unstemmed |
Estimation of Surface Water Availability for Shihmen Reservoir located in Taiwan |
title_sort |
estimation of surface water availability for shihmen reservoir located in taiwan |
publishDate |
2010 |
url |
http://ndltd.ncl.edu.tw/handle/42771180469815464406 |
work_keys_str_mv |
AT pojuikung estimationofsurfacewateravailabilityforshihmenreservoirlocatedintaiwan AT gōngbǎiruì estimationofsurfacewateravailabilityforshihmenreservoirlocatedintaiwan AT pojuikung shíménshuǐkùshàngyóujíshuǐqūdemiànshuǐqiánnéngshuǐliàngtuīgūzhīyánjiū AT gōngbǎiruì shíménshuǐkùshàngyóujíshuǐqūdemiànshuǐqiánnéngshuǐliàngtuīgūzhīyánjiū |
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