ClimateSearch

London, Ontario

Canada · 422k people · 249 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 high29°F (-1°C)31°F (0°C)41°F (5°C)54°F (12°C)66°F (19°C)75°F (24°C)79°F (26°C)77°F (25°C)71°F (21°C)58°F (14°C)45°F (7°C)35°F (2°C)
Average low16°F (-9°C)15°F (-9°C)24°F (-4°C)36°F (2°C)48°F (9°C)58°F (15°C)63°F (17°C)62°F (17°C)56°F (13°C)45°F (7°C)34°F (1°C)24°F (-4°C)
Dew point17°F (-9°C)16°F (-9°C)23°F (-5°C)33°F (1°C)46°F (8°C)56°F (13°C)60°F (16°C)60°F (16°C)54°F (12°C)43°F (6°C)32°F (0°C)23°F (-5°C)
Rainfall2.9 in (73 mm)2.3 in (59 mm)2.7 in (70 mm)3.7 in (93 mm)3.8 in (97 mm)4 in (101 mm)4 in (102 mm)3.3 in (83 mm)3.4 in (86 mm)3.4 in (86 mm)3.1 in (78 mm)2.7 in (69 mm)
Rainy days121011121212121110121212
Snowfall10.4 in (26.3 cm)9 in (22.8 cm)6.4 in (16.3 cm)2.4 in (6.1 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.5 cm)3.6 in (9.1 cm)9.1 in (23 cm)
Sunshine155 h189 h250 h276 h338 h372 h396 h354 h297 h229 h168 h138 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 (+1.8°C)

Models range from +2.4°F (+1.4°C) to +4.0°F (+2.2°C)

Days above 90°F (32°C) a year

1 2

About 2.2× as many

Warming by month
  • January: +3.9°F (+2.2°C)
  • February: +3.6°F (+2.0°C)
  • March: +4.0°F (+2.2°C)
  • April: +3.1°F (+1.7°C)
  • May: +3.7°F (+2.0°C)
  • June: +2.9°F (+1.6°C)
  • July: +3.5°F (+1.9°C)
  • August: +3.5°F (+2.0°C)
  • September: +3.4°F (+1.9°C)
  • October: +2.8°F (+1.6°C)
  • November: +3.6°F (+2.0°C)
  • December: +3.1°F (+1.7°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.