ClimateSearch

St. John's, Newfoundland and Labrador

Canada · 111k people · 42 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 high32°F (0°C)32°F (0°C)36°F (2°C)44°F (7°C)54°F (12°C)63°F (17°C)72°F (22°C)72°F (22°C)65°F (18°C)55°F (13°C)46°F (8°C)37°F (3°C)
Average low19°F (-7°C)19°F (-7°C)23°F (-5°C)30°F (-1°C)37°F (3°C)45°F (7°C)54°F (12°C)55°F (13°C)49°F (9°C)41°F (5°C)33°F (1°C)26°F (-4°C)
Dew point20°F (-6°C)20°F (-7°C)23°F (-5°C)30°F (-1°C)37°F (3°C)45°F (7°C)54°F (12°C)56°F (13°C)50°F (10°C)42°F (5°C)34°F (1°C)26°F (-3°C)
Rainfall6 in (153 mm)5 in (128 mm)5 in (128 mm)4.9 in (123 mm)4.2 in (108 mm)3.9 in (99 mm)4.2 in (108 mm)4.1 in (105 mm)4.7 in (119 mm)6.1 in (155 mm)5.7 in (146 mm)6.6 in (168 mm)
Rainy days14131212111110910131315
Snowfall21.9 in (55.6 cm)18.7 in (47.6 cm)15.9 in (40.4 cm)8.3 in (21.2 cm)1.6 in (4.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.4 in (1.1 cm)4.8 in (12.3 cm)15.9 in (40.5 cm)
Sunshine62 h71 h104 h110 h126 h123 h149 h146 h127 h90 h60 h49 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

+2.0°F (+1.1°C)

Models range from +1.6°F (+0.9°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +3.3°F (+1.8°C)
  • February: +3.0°F (+1.7°C)
  • March: +2.4°F (+1.3°C)
  • April: +1.8°F (+1.0°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.0°F (+1.1°C)
  • August: +1.7°F (+0.9°C)
  • September: +2.3°F (+1.3°C)
  • October: +2.5°F (+1.4°C)
  • November: +3.0°F (+1.7°C)
  • December: +2.8°F (+1.6°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.