ClimateSearch

Sydney, Nova Scotia

Canada · 106k people · 9 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 high31°F (0°C)31°F (-1°C)36°F (2°C)45°F (7°C)56°F (13°C)65°F (19°C)74°F (23°C)74°F (24°C)67°F (20°C)56°F (14°C)47°F (8°C)38°F (3°C)
Average low18°F (-8°C)15°F (-9°C)22°F (-6°C)31°F (-1°C)39°F (4°C)48°F (9°C)56°F (14°C)58°F (15°C)51°F (11°C)43°F (6°C)34°F (1°C)26°F (-3°C)
Dew point19°F (-7°C)17°F (-8°C)22°F (-5°C)31°F (-1°C)40°F (4°C)49°F (10°C)58°F (15°C)59°F (15°C)53°F (12°C)43°F (6°C)35°F (1°C)26°F (-3°C)
Rainfall5.8 in (148 mm)5.4 in (138 mm)5.4 in (137 mm)5 in (126 mm)4.2 in (107 mm)4.2 in (106 mm)4 in (102 mm)3.9 in (98 mm)4.8 in (122 mm)6.2 in (159 mm)5.9 in (150 mm)6.3 in (161 mm)
Rainy days131112121110989121213
Snowfall19.4 in (49.4 cm)18.5 in (47 cm)15 in (38.1 cm)9.7 in (24.6 cm)0.7 in (1.7 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.4 cm)3.6 in (9.2 cm)14.9 in (37.8 cm)
Sunshine57 h87 h127 h140 h164 h179 h200 h202 h163 h117 h66 h46 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

+2.6°F (+1.5°C)

Models range from +2.0°F (+1.1°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +3.8°F (+2.1°C)
  • February: +4.4°F (+2.4°C)
  • March: +2.9°F (+1.6°C)
  • April: +3.3°F (+1.8°C)
  • May: +3.3°F (+1.8°C)
  • June: +2.8°F (+1.6°C)
  • July: +3.0°F (+1.7°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.6°F (+1.5°C)
  • November: +3.5°F (+2.0°C)
  • December: +3.9°F (+2.2°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.