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Observations sur l'influence hydrologique de la neige dans l'Est du Canada

Bibliographic Data

ID3827646
AuthorsChristian Mingasson (corresponding author)
Year2005
Volume2
Issue3
Pages75-86
Publication date2005-04-12
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenueCahiers de géographie du Québec (JOURNAL)
Journal identifiersISSN: 0007-9766 • E-ISSN: 1708-8968
PublisherConsortium Erudit (PUBLISHER • CA)
DOI10.7202/020063ar
OpenAlexW2171035235
LanguageFR
Citations received1

This article deals with a group of 27 rivers all situated East of the 85 th meridian and South of Hudson Bay. In the first place, the author bas calculated the ratios of snow run-off during the springtime discharge. In the Maritime Provinces, the ratio obtained is only 20% of the total discharge (with a minimum of 17%) because of the rainy marine characteristics of the climate. In the Laurentian region, the ratio is close to 30% (maximum 35%) because of abundant snow precipitations and quite low summer discharge. One must note the retentional influence of lakes which display the flooding period jar beyond springtime and lower the spring ratio down to 23%. For instance, in Northern Ontario, due to losses in the marshy zones, the author bas found a ratio of only 19%. A second problem raised in this paper is the dating of the beginning of floods caused by the melting of snow. In the Southern parts of the Maritime provinces and of Ontario, the waters are high on April 5 th. In the Southern and Central parts of Québec, the flooding period begins between the 6 th and the 20 th of April. In the regions situated North of the St. Lawrence and South of James Bay, the flooding period usually begins after the 25 th of April. So the flooding period caused by the melting of snow happens later in the Northern regions. Finally, the author considers the monthly ratios of discharge during the month that knows the highest waters. Those ratios are between 2 and 3 (maximum 4.64) but they can lower down to 1.50 due to retention operated by the lakes. The month of maximum flooding extends from March, in the Southern parts of the zone covered by this study, to June, in the Northern parts. As a general rule, the figures found in this article are lower than those recorded for the rivers of the U.S.S.R

Bay · Flooding (psychology) · Geography · Hydrology (agriculture) · Meteorology · Period (music) · Physical geography · Snow · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Geology · Hydrology and Watershed Management Studies · Oceanography

  • L'hydrologie printanière de la rivière Saint-François

    Pierre Cazalis•Cahiers de géographie du Québec•2005

Unique citing works1
Citations per year0,05
Citation span2005 - 2005 (1)
Citation velocityhistorical
Highly citedNo

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Open DOISci-HubOpen Access
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