Investigation of Groundwater Contribution to Stream Flow under Climate and Land Use Changes: A Case Study in British Columbia, Canada

G. Saha
{"title":"Investigation of Groundwater Contribution to Stream Flow under Climate and Land Use Changes: A Case Study in British Columbia, Canada","authors":"G. Saha","doi":"10.9734/BJECC/2015/14218","DOIUrl":null,"url":null,"abstract":"Groundwater contributes a significant proportion of stream flow, and its contribution varies temporally throughout the year. The objective of this study was to investigate the temporal dynamics of groundwater contribution to stream flow under the effects of climate and land use changes. A study area of the Mainstem sub-watershed of the Kiskatinaw River watershed, British Columbia, Canada was used as a case study. A physically conceptual model, Gridded Surface Subsurface Hydrologic Analysis (GSSHA), was developed for the study area. One greenhouse gas (GHG) emission scenario (i.e., B1: more integrated and environmental friendly world) was used for climate change study for 2012-2016, and land use changes scenarios were generated for shortterm period (2012-2016) due to limited future projected land use data. The simulation results revealed that climate change affects significantly the temporal patterns of mean groundwater contribution to stream flow. Due to precipitation variability, these contributions varied monthly, seasonally, and annually. When land use changes (i.e., increasing forest clear cut area, and decreasing forest and agricultural areas) were combined with climate change scenarios, these contributions were decreased due to changes in the flow patterns to the regime with more surface runoff and stream flow but less groundwater discharge. Compared to the reference period (20072011), the mean annual groundwater contribution to stream flow from 2012 to 2016 under the B1 climate change scenario and the combined effects of B1 scenario and land use changes is expected to decrease by 1.8% and 4.3%, respectively, due to increased precipitation (on average 3.6% under the B1 scenario) and temperature (on average 0.36°C under the B1 scenario), and land use changes. The results obtained from this study will provide useful information for seasonal and annual water extractions from the river and allocation to the stakeholders for future water Original Research Article Saha; BJECC, 5(1): 1-22, 2015; Article no.BJECC.2015.001 2 supply, as well as ecological conditions of the stream, which will be beneficial to aquatic ecosystems. They will also provide how land use changes can impact the groundwater contribution to stream flow, which will be useful for planning of water resources management considering future climate and land use changes.","PeriodicalId":373103,"journal":{"name":"British Journal of Environment and Climate Change","volume":"126 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2015-01-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"British Journal of Environment and Climate Change","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.9734/BJECC/2015/14218","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

Groundwater contributes a significant proportion of stream flow, and its contribution varies temporally throughout the year. The objective of this study was to investigate the temporal dynamics of groundwater contribution to stream flow under the effects of climate and land use changes. A study area of the Mainstem sub-watershed of the Kiskatinaw River watershed, British Columbia, Canada was used as a case study. A physically conceptual model, Gridded Surface Subsurface Hydrologic Analysis (GSSHA), was developed for the study area. One greenhouse gas (GHG) emission scenario (i.e., B1: more integrated and environmental friendly world) was used for climate change study for 2012-2016, and land use changes scenarios were generated for shortterm period (2012-2016) due to limited future projected land use data. The simulation results revealed that climate change affects significantly the temporal patterns of mean groundwater contribution to stream flow. Due to precipitation variability, these contributions varied monthly, seasonally, and annually. When land use changes (i.e., increasing forest clear cut area, and decreasing forest and agricultural areas) were combined with climate change scenarios, these contributions were decreased due to changes in the flow patterns to the regime with more surface runoff and stream flow but less groundwater discharge. Compared to the reference period (20072011), the mean annual groundwater contribution to stream flow from 2012 to 2016 under the B1 climate change scenario and the combined effects of B1 scenario and land use changes is expected to decrease by 1.8% and 4.3%, respectively, due to increased precipitation (on average 3.6% under the B1 scenario) and temperature (on average 0.36°C under the B1 scenario), and land use changes. The results obtained from this study will provide useful information for seasonal and annual water extractions from the river and allocation to the stakeholders for future water Original Research Article Saha; BJECC, 5(1): 1-22, 2015; Article no.BJECC.2015.001 2 supply, as well as ecological conditions of the stream, which will be beneficial to aquatic ecosystems. They will also provide how land use changes can impact the groundwater contribution to stream flow, which will be useful for planning of water resources management considering future climate and land use changes.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
气候和土地利用变化下地下水对河流流量的贡献研究——以加拿大不列颠哥伦比亚省为例
地下水占河流流量的很大比例,其贡献在一年中的时间上是不同的。本研究旨在探讨气候和土地利用变化影响下地下水对河流流量贡献的时间动态。加拿大不列颠哥伦比亚省基斯卡蒂诺河流域主干分流域的一个研究区被用作个案研究。为研究区开发了一个物理概念模型——网格地表地下水文分析(GSSHA)。2012-2016年气候变化研究采用了一个温室气体(GHG)排放情景(即B1:更加一体化和环境友好型世界),由于未来土地利用预测数据有限,生成了短期(2012-2016年)的土地利用变化情景。模拟结果表明,气候变化显著影响了平均地下水对河流流量贡献的时间格局。由于降水变率,这些贡献每月、季节和每年都有所不同。当土地利用变化(即森林砍伐面积增加,森林和农业面积减少)与气候变化情景相结合时,由于地表径流和河流流量增加而地下水流量减少的流动模式的变化,这些贡献减少。与参考期(2007 - 2011年)相比,在B1气候变化情景下以及B1情景与土地利用变化的综合影响下,2012 - 2016年地下水对河流流量的年平均贡献预计分别减少1.8%和4.3%,主要原因是降水增加(B1情景下平均增加3.6%)、气温增加(B1情景下平均增加0.36℃)以及土地利用变化。本研究的结果将为今后从河流中提取季节性和年度水资源以及分配给利益相关者提供有用的信息。生物工程学报,5(1):1-22,2015;Article no.BJECC.2015.001 2供应,以及溪流的生态条件,这将有利于水生生态系统。它们还将提供土地利用变化如何影响地下水对水流的贡献,这将有助于考虑到未来气候和土地利用变化的水资源管理规划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Modelling of Soil Loss through RUSLE2 for Soil Management in an Agricultural Field of Uccle, Belgium Characterization of Particulate Matter in Urban Environments and Its Effects on the Respiratory System of Mice Detecting Non-negligible New Influences in Environmental Data via a General Spatio-temporal Autoregressive Model Estimating surface CO2 flux based on soil concentration profile Response of Pigeonpea (Cajanus cajan L.) to Seed Polymerization with Micronutrients and Foliar Spray at Different Growth Stages
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1