Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use

We compared the spatiotemporal variability of temperatures and precipitation with that of the magnitude and timing of maximum daily spring flows in the geographically adjacent L’Assomption River (agricultural) and Matawin River (forested) watersheds during the period from 1932 to 2013. With regard t...

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Main Authors: Ali A. Assani, Raphaëlle Landry, Christophe Kinnard, Ouassila Azouaoui, Christine Demers, Karine Lacasse
Format: Article
Language:English
Published: Wiley 2016-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2016/3746460
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author Ali A. Assani
Raphaëlle Landry
Christophe Kinnard
Ouassila Azouaoui
Christine Demers
Karine Lacasse
author_facet Ali A. Assani
Raphaëlle Landry
Christophe Kinnard
Ouassila Azouaoui
Christine Demers
Karine Lacasse
author_sort Ali A. Assani
collection DOAJ
description We compared the spatiotemporal variability of temperatures and precipitation with that of the magnitude and timing of maximum daily spring flows in the geographically adjacent L’Assomption River (agricultural) and Matawin River (forested) watersheds during the period from 1932 to 2013. With regard to spatial variability, fall, winter, and spring temperatures as well as total precipitation are higher in the agricultural watershed than in the forested one. The magnitude of maximum daily spring flows is also higher in the first watershed as compared with the second, owing to substantial runoff, given that the amount of snow that gives rise to these flows is not significantly different in the two watersheds. These flows occur early in the season in the agricultural watershed because of the relatively high temperatures. With regard to temporal variability, minimum temperatures increased over time in both watersheds. Maximum temperatures in the fall only increased in the agricultural watershed. The amount of spring rain increased over time in both watersheds, whereas total precipitation increased significantly in the agricultural watershed only. However, the amount of snow decreased in the forested watershed. The magnitude of maximum daily spring flows increased over time in the forested watershed.
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institution Kabale University
issn 1687-9309
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publishDate 2016-01-01
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series Advances in Meteorology
spelling doaj-art-0fcc63c3862a485cb318a7af584fc6022025-02-03T05:53:41ZengWileyAdvances in Meteorology1687-93091687-93172016-01-01201610.1155/2016/37464603746460Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land UseAli A. Assani0Raphaëlle Landry1Christophe Kinnard2Ouassila Azouaoui3Christine Demers4Karine Lacasse5Department of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaDepartment of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaDepartment of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaDepartment of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaDepartment of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaDepartment of Environmental Sciences, University of Quebec at Trois-Rivières, 3351 Boulevard of the Forges, Trois-Rivières, QC, G9A 5H7, CanadaWe compared the spatiotemporal variability of temperatures and precipitation with that of the magnitude and timing of maximum daily spring flows in the geographically adjacent L’Assomption River (agricultural) and Matawin River (forested) watersheds during the period from 1932 to 2013. With regard to spatial variability, fall, winter, and spring temperatures as well as total precipitation are higher in the agricultural watershed than in the forested one. The magnitude of maximum daily spring flows is also higher in the first watershed as compared with the second, owing to substantial runoff, given that the amount of snow that gives rise to these flows is not significantly different in the two watersheds. These flows occur early in the season in the agricultural watershed because of the relatively high temperatures. With regard to temporal variability, minimum temperatures increased over time in both watersheds. Maximum temperatures in the fall only increased in the agricultural watershed. The amount of spring rain increased over time in both watersheds, whereas total precipitation increased significantly in the agricultural watershed only. However, the amount of snow decreased in the forested watershed. The magnitude of maximum daily spring flows increased over time in the forested watershed.http://dx.doi.org/10.1155/2016/3746460
spellingShingle Ali A. Assani
Raphaëlle Landry
Christophe Kinnard
Ouassila Azouaoui
Christine Demers
Karine Lacasse
Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
Advances in Meteorology
title Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
title_full Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
title_fullStr Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
title_full_unstemmed Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
title_short Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use
title_sort comparison of the spatiotemporal variability of temperature precipitation and maximum daily spring flows in two watersheds in quebec characterized by different land use
url http://dx.doi.org/10.1155/2016/3746460
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