ClimateSearch

Rochester, New York

United States · 210k people · 153 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)33°F (1°C)40°F (5°C)52°F (11°C)64°F (18°C)73°F (23°C)79°F (26°C)78°F (25°C)71°F (22°C)59°F (15°C)47°F (8°C)37°F (3°C)
Average low20°F (-7°C)19°F (-7°C)26°F (-3°C)37°F (3°C)48°F (9°C)59°F (15°C)65°F (18°C)64°F (18°C)58°F (14°C)47°F (8°C)36°F (2°C)27°F (-3°C)
Dew point18°F (-8°C)18°F (-8°C)24°F (-5°C)34°F (1°C)46°F (8°C)56°F (13°C)61°F (16°C)60°F (16°C)54°F (12°C)44°F (6°C)33°F (1°C)24°F (-4°C)
Rainfall3.3 in (83 mm)2.6 in (65 mm)3.1 in (79 mm)3.9 in (99 mm)3.2 in (82 mm)3.5 in (89 mm)3.5 in (88 mm)3.1 in (80 mm)3.4 in (87 mm)4.2 in (106 mm)3.7 in (95 mm)3.7 in (93 mm)
Rainy days151112121112111211131416
Snowfall13.5 in (34.2 cm)10.9 in (27.8 cm)8.7 in (22.2 cm)2.8 in (7 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)4.7 in (11.9 cm)11.5 in (29.1 cm)
Sunshine152 h184 h247 h271 h339 h354 h384 h353 h287 h222 h165 h133 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

+2.7°F (+1.5°C)

Models range from +1.9°F (+1.1°C) to +3.7°F (+2.0°C)

Days above 90°F (32°C) a year

1 2

About 1.6× as many

Warming by month
  • January: +4.1°F (+2.3°C)
  • February: +3.9°F (+2.2°C)
  • March: +3.5°F (+2.0°C)
  • April: +2.8°F (+1.6°C)
  • May: +3.8°F (+2.1°C)
  • June: +2.9°F (+1.6°C)
  • July: +2.6°F (+1.4°C)
  • August: +2.7°F (+1.5°C)
  • September: +2.8°F (+1.6°C)
  • October: +3.1°F (+1.7°C)
  • November: +3.3°F (+1.9°C)
  • December: +3.0°F (+1.7°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.