The Changes of Stream Discharge under Low-flow Season

碩士 === 國立彰化師範大學 === 地理學系 === 103 === Stream flow is vital to human life and terrestrial ecosystem, especially under low-flow season; it turns into a critical factor for water supply capability, water quality control and aquatic habitat sustainability. In Taiwan, recent reports indicate a general tre...

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Main Authors: Mei- Chih Lin, 林美志
Other Authors: Shih- Chien Chan
Format: Others
Language:zh-TW
Published: 2015
Online Access:http://ndltd.ncl.edu.tw/handle/62121985194798292977
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spelling ndltd-TW-103NCUE51360142016-08-14T04:11:19Z http://ndltd.ncl.edu.tw/handle/62121985194798292977 The Changes of Stream Discharge under Low-flow Season 河川低流量特性變動之研究 Mei- Chih Lin 林美志 碩士 國立彰化師範大學 地理學系 103 Stream flow is vital to human life and terrestrial ecosystem, especially under low-flow season; it turns into a critical factor for water supply capability, water quality control and aquatic habitat sustainability. In Taiwan, recent reports indicate a general trend of increasing drought frequency, leading the stability of water resource in dry season to a highly concerned issue. This study aims to access changes of stream discharge under low-flow season and the relations with watershed parameters as the discussion of this link is still limited. Daily rainfall and stream flow records of 6 watersheds in Dahan River and Xindian Creek for 1970 to 2010 are analyzed in this study. All records are firstly divided equally into two periods and long term variations of low-flow are later drawn out through statistic analysis of flow duration curve (FDC) and frequency analysis (FA). The study reveals mean daily flow under low-flow season is decreasing except for Fu Shan, and the initial month of the season varies in watersheds. Through flow duration curve analysis, the flow discharge of San Hsia and Kao Yi stations are found decreasing under Q90 percentile while others increasing. At last the 100 year low-flow discharge dramatically declines on San Hsia, Kao Yi and Ching Mei stations, on the contrary Fu Shan is going up. The result indicates the changes of low-flow discharge are not unanimous in Danshui river basin because of diverse environmental characteristics in watersheds.Weak northeast monsoon caused by climate change has given rise to rainfall variances on watershed and could be responsible for less rainfall on Dahan river in low-flow season.Changes of land use over time lead to low-flow variation. Urbanization and water withdrawal affect extreme low-flow transform on San Hsia and Ching Mei. We believe rainfall variances, land use types, urbanization and water withdrawal are factors relating to changes of stream discharge under low-flow season. Shih- Chien Chan 詹仕堅 2015 學位論文 ; thesis 70 zh-TW
collection NDLTD
language zh-TW
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description 碩士 === 國立彰化師範大學 === 地理學系 === 103 === Stream flow is vital to human life and terrestrial ecosystem, especially under low-flow season; it turns into a critical factor for water supply capability, water quality control and aquatic habitat sustainability. In Taiwan, recent reports indicate a general trend of increasing drought frequency, leading the stability of water resource in dry season to a highly concerned issue. This study aims to access changes of stream discharge under low-flow season and the relations with watershed parameters as the discussion of this link is still limited. Daily rainfall and stream flow records of 6 watersheds in Dahan River and Xindian Creek for 1970 to 2010 are analyzed in this study. All records are firstly divided equally into two periods and long term variations of low-flow are later drawn out through statistic analysis of flow duration curve (FDC) and frequency analysis (FA). The study reveals mean daily flow under low-flow season is decreasing except for Fu Shan, and the initial month of the season varies in watersheds. Through flow duration curve analysis, the flow discharge of San Hsia and Kao Yi stations are found decreasing under Q90 percentile while others increasing. At last the 100 year low-flow discharge dramatically declines on San Hsia, Kao Yi and Ching Mei stations, on the contrary Fu Shan is going up. The result indicates the changes of low-flow discharge are not unanimous in Danshui river basin because of diverse environmental characteristics in watersheds.Weak northeast monsoon caused by climate change has given rise to rainfall variances on watershed and could be responsible for less rainfall on Dahan river in low-flow season.Changes of land use over time lead to low-flow variation. Urbanization and water withdrawal affect extreme low-flow transform on San Hsia and Ching Mei. We believe rainfall variances, land use types, urbanization and water withdrawal are factors relating to changes of stream discharge under low-flow season.
author2 Shih- Chien Chan
author_facet Shih- Chien Chan
Mei- Chih Lin
林美志
author Mei- Chih Lin
林美志
spellingShingle Mei- Chih Lin
林美志
The Changes of Stream Discharge under Low-flow Season
author_sort Mei- Chih Lin
title The Changes of Stream Discharge under Low-flow Season
title_short The Changes of Stream Discharge under Low-flow Season
title_full The Changes of Stream Discharge under Low-flow Season
title_fullStr The Changes of Stream Discharge under Low-flow Season
title_full_unstemmed The Changes of Stream Discharge under Low-flow Season
title_sort changes of stream discharge under low-flow season
publishDate 2015
url http://ndltd.ncl.edu.tw/handle/62121985194798292977
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