ClimateSearch

Washington, District of Columbia

United States · 690k people · 12 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 high43°F (6°C)46°F (8°C)55°F (13°C)66°F (19°C)74°F (24°C)83°F (29°C)88°F (31°C)85°F (30°C)79°F (26°C)67°F (20°C)56°F (13°C)47°F (8°C)
Average low28°F (-2°C)29°F (-2°C)36°F (2°C)46°F (8°C)56°F (13°C)65°F (18°C)70°F (21°C)69°F (21°C)62°F (17°C)51°F (10°C)40°F (5°C)32°F (0°C)
Dew point24°F (-4°C)25°F (-4°C)32°F (0°C)43°F (6°C)53°F (12°C)62°F (17°C)66°F (19°C)65°F (19°C)60°F (15°C)49°F (9°C)37°F (3°C)29°F (-1°C)
Rainfall3.1 in (79 mm)2.9 in (74 mm)3.9 in (99 mm)3.4 in (87 mm)4 in (101 mm)3.6 in (91 mm)4.4 in (111 mm)3.8 in (98 mm)4.6 in (117 mm)3.5 in (89 mm)3 in (77 mm)3.6 in (91 mm)
Rainy days9910111112121010889
Snowfall5.1 in (12.9 cm)5.4 in (13.6 cm)3.4 in (8.6 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.1 in (0.2 cm)0.3 in (0.7 cm)2.8 in (7.1 cm)
Sunshine205 h213 h256 h283 h324 h345 h365 h337 h277 h248 h215 h198 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 +2.4°F (+1.4°C) to +3.7°F (+2.0°C)

Days above 90°F (32°C) a year

27 48

About 1.8× as many

Warming by month
  • January: +3.9°F (+2.1°C)
  • February: +3.6°F (+2.0°C)
  • March: +3.7°F (+2.1°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.8°F (+1.6°C)
  • June: +3.0°F (+1.7°C)
  • July: +3.4°F (+1.9°C)
  • August: +3.0°F (+1.7°C)
  • September: +2.8°F (+1.5°C)
  • October: +3.1°F (+1.7°C)
  • November: +3.1°F (+1.7°C)
  • December: +2.7°F (+1.5°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.