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Snow cover variability in Qu\u00e9bec was found to be significantly correlated with most of the major atmospheric circulation patterns affecting the climate of eastern North America but the influence was characterized by strong multidecadal\u2010scale variability. The strongest and most consistent relationship was observed between the Pacific Decadal Oscillation (PDO) and fall SCD variability over western Qu\u00e9bec. El Ni\u00f1o\u2010Southern Oscillation (ENSO) was found to have a limited impact on Qu\u00e9bec snow cover. Evidence was found for a shift in circulation over the study region around 1980 associated with an abrupt increase in sea level pressure (SLP) and decreases in winter precipitation, snow depth and SWE over much of southern Qu\u00e9bec, as well as changes in the atmospheric patterns with significant links to snow cover variability. Trend analysis of the reconstructed snow cover over 1948\u20132005 provided evidence of a clear north\u2013south gradient in SWEmax and spring SCD with significant local decreases over southern Qu\u00e9bec and significant local increases over north\u2010central Qu\u00e9bec. The increase in SWEmax over northern Qu\u00e9bec is consistent with proxy data (lake levels, tree growth forms, permafrost temperatures), with hemispheric\u2010wide trends of increasing precipitation over higher latitudes, and with projections of global climate models (GCMs). Copyright \u00a9 2010 Her Majesty the Queen in right of Canada. Published by John Wiley &amp; Sons. 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