Investigation of Long-Term Climate and Streamflow Patterns in Ontario
Amin Azarkhish, R. Rudra, P. Daggupati, J. Dhiman, T. Dickinson, P. Goel
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引用次数: 2
Abstract
To develop mitigation and adaptation strategies for undesired consequences of climate change, it is important to understand the changing hydrological and climatological trends in the past few decades. Although the changing climate is a cause of concern for the entire planet, its effects can vary significantly on a regional scale. Canada has experienced a rapid rise in the annual mean surface air temperature in the past decades. The current study aims to investigate trends in monthly mean precipitation, rainfall, snowfall, maximum and minimum temperature, as well as baseflow, surface runoff, and total streamflow values for the province of Ontario, Canada. To the best of the author’s knowledge, a similar study involving rural and urban watersheds, that quantifies the impact of changing climate on temperature and other hydrological processes over a period ranging from 1968 to 2017, has not yet been conducted for Ontario. Man-Kendall trend test was used to analyze trends in the above mentioned climatic and hydrometric parameters for rural and urban watersheds situated in the northern and southern parts of Ontario. The results of this study indicate that the mean monthly minimum temperatures for rural watersheds situated in southern Ontario have increased significantly for the winter and summer months, which may have caused an increase in snowmelt and consequently the streamflow for the winter months in the region. Unlike the watersheds in southern Ontario, the northern watersheds witnessed relatively fewer instances of significant changes in mean monthly temperatures, and in some cases, declining rates have been noted. Similarly, only a few watersheds in the north saw a substantial drop in baseflow over the summer months. For nearly all the months, the average monthly minimum and maximum temperatures were found to increase for urban watersheds. The streamflow, baseflow, and surface runoff increased, likely due to rapid urbanization, resulting in a lower infiltration rate. These results will contriHow to cite this paper: Azarkhish, A., Rudra, R., Daggupati, P., Dhiman, J., Dickinson, T., & Goel, P. (2021). Investigation of Long-Term Climate and Streamflow Patterns in Ontario. American Journal of Climate Change, 10, 467-489. https://doi.org/10.4236/ajcc.2021.104024 Received: June 28, 2021 Accepted: December 14, 2021 Published: December 17, 2021 Copyright © 2021 by author(s) and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Open Access
安大略省长期气候和水流模式的调查
为了制定缓解和适应气候变化不良后果的战略,必须了解过去几十年来不断变化的水文和气候趋势。尽管气候变化是整个地球关注的一个原因,但其影响在区域范围内可能有很大差异。在过去的几十年里,加拿大经历了年平均地表气温的快速上升。目前的研究旨在调查加拿大安大略省的月平均降水量、降雨量、降雪量、最高和最低温度以及基流、地表径流和总流值的趋势。据作者所知,安大略省尚未进行过一项涉及农村和城市流域的类似研究,该研究量化了1968年至2017年期间气候变化对温度和其他水文过程的影响。Man-Kendall趋势检验用于分析安大略省北部和南部农村和城市流域上述气候和水文参数的趋势。本研究结果表明,位于安大略省南部农村流域的月平均最低气温在冬季和夏季显著增加,这可能导致该地区冬季融雪量增加,从而导致该地区的河流流量增加。与安大略省南部的流域不同,北部流域的月平均气温发生显著变化的情况相对较少,在某些情况下,已经注意到下降的速度。同样,在夏季的几个月里,只有北部的几个流域的基本流量出现了大幅下降。几乎所有月份,城市流域的月平均最低和最高气温都有所上升。径流、基流和地表径流增加,可能是由于快速城市化,导致入渗速率降低。这些结果将有助于如何引用本文:Azarkhish, A., Rudra, R., Daggupati, P., Dhiman, J., Dickinson, T., & Goel, P.(2021)。安大略省长期气候和水流模式的调查。气候变化学报,10,467-489。https://doi.org/10.4236/ajcc.2021.104024收稿日期:2021年6月28日收稿日期:2021年12月14日出版日期:2021年12月17日版权所有©作者与科研出版公司。本作品采用知识共享署名国际许可协议(CC BY 4.0)。http://creativecommons.org/licenses/by/4.0/开放获取
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