ClimateSearch

Trois-Rivières, Quebec

Canada · 144k people · 18 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high20°F (-6°C)24°F (-4°C)35°F (2°C)49°F (10°C)64°F (18°C)73°F (23°C)77°F (25°C)75°F (24°C)67°F (20°C)54°F (12°C)40°F (5°C)28°F (-2°C)
Average low4°F (-15°C)8°F (-13°C)18°F (-8°C)32°F (0°C)46°F (8°C)57°F (14°C)62°F (17°C)61°F (16°C)53°F (12°C)41°F (5°C)29°F (-2°C)13°F (-10°C)
Dew point6°F (-15°C)8°F (-13°C)18°F (-8°C)29°F (-2°C)43°F (6°C)54°F (12°C)60°F (15°C)59°F (15°C)51°F (11°C)39°F (4°C)27°F (-3°C)14°F (-10°C)
Rainfall3 in (77 mm)2.4 in (62 mm)2.9 in (75 mm)3.8 in (97 mm)3.8 in (97 mm)4.2 in (108 mm)4.5 in (114 mm)4.3 in (109 mm)3.9 in (100 mm)4.4 in (111 mm)3.5 in (89 mm)3.5 in (90 mm)
Rainy days11911121213141211111212
Snowfall14.3 in (36.3 cm)13.4 in (34 cm)11.5 in (29.2 cm)5 in (12.8 cm)0.2 in (0.4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.9 in (2.2 cm)6.3 in (16.1 cm)14.9 in (37.8 cm)
Sunshine175 h194 h253 h264 h319 h339 h368 h343 h267 h212 h162 h150 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+3.3°F (+1.9°C)

Models range from +2.4°F (+1.3°C) to +4.0°F (+2.2°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +5.1°F (+2.8°C)
  • February: +4.5°F (+2.5°C)
  • March: +3.0°F (+1.7°C)
  • April: +4.0°F (+2.2°C)
  • May: +3.9°F (+2.1°C)
  • June: +2.8°F (+1.6°C)
  • July: +3.6°F (+2.0°C)
  • August: +3.6°F (+2.0°C)
  • September: +3.3°F (+1.9°C)
  • October: +2.4°F (+1.3°C)
  • November: +4.3°F (+2.4°C)
  • December: +5.2°F (+2.9°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.