ClimateSearch

Whalley, British Columbia

Canada · 103k people · 85 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 high44°F (7°C)48°F (9°C)52°F (11°C)58°F (14°C)65°F (18°C)69°F (21°C)76°F (24°C)76°F (24°C)69°F (21°C)58°F (14°C)49°F (10°C)44°F (7°C)
Average low34°F (1°C)35°F (2°C)38°F (3°C)42°F (6°C)48°F (9°C)53°F (12°C)57°F (14°C)57°F (14°C)51°F (11°C)44°F (7°C)38°F (4°C)35°F (2°C)
Dew point32°F (0°C)32°F (0°C)36°F (2°C)40°F (4°C)46°F (8°C)50°F (10°C)54°F (12°C)55°F (13°C)52°F (11°C)45°F (7°C)38°F (3°C)32°F (0°C)
Rainfall10.6 in (269 mm)5.1 in (130 mm)6.5 in (164 mm)5.2 in (133 mm)3.6 in (91 mm)3.1 in (79 mm)1.7 in (43 mm)2.3 in (59 mm)2.9 in (74 mm)7 in (178 mm)11.1 in (282 mm)8.4 in (213 mm)
Rainy days181417151110568151918
Snowfall14.4 in (36.7 cm)11.5 in (29.1 cm)10.2 in (25.9 cm)2 in (5.2 cm)0.2 in (0.4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.5 cm)6.7 in (16.9 cm)19.2 in (48.8 cm)
Sunshine56 h87 h114 h158 h206 h217 h286 h258 h195 h107 h56 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

+2.4°F (+1.4°C)

Models range from +1.9°F (+1.1°C) to +3.0°F (+1.7°C)

Days above 90°F (32°C) a year

1 → 1

About 1.8× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.1°F (+0.6°C)
  • March: +2.0°F (+1.1°C)
  • April: +1.2°F (+0.6°C)
  • May: +1.4°F (+0.8°C)
  • June: +2.8°F (+1.6°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.3°F (+1.3°C)
  • October: +2.4°F (+1.3°C)
  • November: +2.5°F (+1.4°C)
  • December: +1.3°F (+0.7°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.