ClimateSearch

North Stamford, Connecticut

United States · 121k people · 67 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 high37°F (3°C)39°F (4°C)46°F (8°C)57°F (14°C)67°F (20°C)77°F (25°C)82°F (28°C)80°F (27°C)73°F (23°C)62°F (17°C)51°F (11°C)42°F (5°C)
Average low24°F (-5°C)24°F (-4°C)31°F (0°C)41°F (5°C)52°F (11°C)62°F (17°C)68°F (20°C)67°F (19°C)61°F (16°C)50°F (10°C)39°F (4°C)31°F (-1°C)
Dew point20°F (-6°C)21°F (-6°C)28°F (-2°C)38°F (3°C)50°F (10°C)59°F (15°C)64°F (18°C)64°F (18°C)58°F (14°C)47°F (8°C)36°F (2°C)27°F (-3°C)
Rainfall3.5 in (89 mm)3.1 in (79 mm)4.2 in (108 mm)3.9 in (98 mm)3.5 in (89 mm)3.9 in (100 mm)3.9 in (100 mm)4.2 in (106 mm)4 in (103 mm)4.2 in (106 mm)3.3 in (84 mm)4.3 in (108 mm)
Rainy days9910111112111199910
Snowfall8.2 in (20.9 cm)8.6 in (21.8 cm)7.6 in (19.3 cm)0.9 in (2.4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.3 in (0.7 cm)1.1 in (2.7 cm)6 in (15.3 cm)
Sunshine202 h211 h258 h275 h312 h333 h362 h337 h277 h243 h199 h182 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

+3.1°F (+1.7°C)

Models range from +2.3°F (+1.3°C) to +4.0°F (+2.2°C)

Days above 90°F (32°C) a year

7 18

About 2.6× as many

Warming by month
  • January: +4.3°F (+2.4°C)
  • February: +3.5°F (+1.9°C)
  • March: +3.7°F (+2.1°C)
  • April: +2.6°F (+1.5°C)
  • May: +3.2°F (+1.8°C)
  • June: +3.1°F (+1.7°C)
  • July: +3.3°F (+1.9°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.0°F (+1.6°C)
  • October: +2.8°F (+1.6°C)
  • November: +3.5°F (+1.9°C)
  • December: +3.2°F (+1.8°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.