Comparison of the interannual variability of spring heavy floods characteristics of tributaries of the St. Lawrence River in Quebec (Canada)

• Published in: Advances in water resources Vol. 35; pp. 110 - 120
• Main Authors: Mazouz, Rabah, Assani, Ali A., Quessy, Jean-François, Légaré, Guillaume
• Format: Journal Article
• Language: English
• Published: Kidlington Elsevier Ltd 2012; Elsevier
• Subjects: Correlation; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Floods; Flow characteristics; Hydrology; Hydrology. Hydrogeology; Kendall tau; Linear regression; Lombard method; Marine; Natural hazards: prediction, damages, etc; Quebec; Rivers; Spring floods; Springs; Springs (elastic); Time measurements; Variance; Water resources; Canada; Quebec; Eastern Canada; Kendall tau; Lombard method; Flow characteristics; Linear regression; Spring floods; Quebec; rivers; tributaries; floods; springs; climate warming; climate; North America; frequency; duration; water resources; correlation; water resource management; streamflow; statistics
• ISSN: 0309-1708; 1872-9657
• DOI: 10.1016/j.advwatres.2011.10.006

► We compare the variability of five characteristics of spring heavy floods in Quebec. ► Changes in the mean and variance of all characteristics of streamflow were observed. ► However, the change in timing is the only one that has a hydroclimatic significance. ► This change is correlated with NAO and AMO.
Comparison of the interannual variability of five characteristics (magnitude, duration, timing, frequency, and variability) of spring heavy floods was carried out for 17 natural rivers in Quebec for the period from 1934 to 2004 to detect any effect of climate warming on these characteristics. This was done using the Lombard method and Copula. Changes in the mean and variance of all characteristics of streamflow were observed, and all these changes are abrupt. Whereas little significant change was observed in the magnitude, duration and variability (CV) series of spring flood flows. A significant change was noted in the frequency (diminution) for five rivers and in the timing of spring floods for six rivers. However, the change in mean timing is the only one that has a hydroclimatic significance in time and space. This change was observed, on the one hand, in the Eastern hydrological region, located on the south shore of the St. Lawrence River, north of 47°N, and characterized by a maritime climate and, on the other hand, in the South-west hydrological region, located on the north shore and characterized by a continental climate. In both cases, the change took place after the second half of the 1970s and is characterized by the early occurrence of spring floods. In addition, in both hydrological regions, the timing of spring floods is correlated with the same hydroclimatic indices, showing a positive correlation with the North Atlantic Oscillation (NAO) and a negative correlation with the Atlantic Multidecadal Oscillation (AMO). Frequency is the only characteristic for which mean and variance changed significantly over time for the same rivers (4), all located north of 48°N, on both shores of the St. Lawrence. For all flow characteristics, the change in variance can predate, postdate or be synchronous with the change in mean. Finally, the dependence between the various characteristics of spring floods as determined using the Kendall tau statistic remained constant in time for most of the rivers.