ClimateSearch

Tuscaloosa, Alabama

United States · 111k people · 68 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 high54°F (12°C)59°F (15°C)66°F (19°C)74°F (23°C)82°F (28°C)88°F (31°C)90°F (32°C)90°F (32°C)86°F (30°C)76°F (25°C)64°F (18°C)56°F (14°C)
Average low38°F (3°C)40°F (5°C)47°F (8°C)54°F (12°C)63°F (17°C)70°F (21°C)74°F (23°C)73°F (23°C)68°F (20°C)57°F (14°C)46°F (8°C)40°F (5°C)
Dew point36°F (2°C)40°F (4°C)46°F (8°C)53°F (12°C)61°F (16°C)68°F (20°C)72°F (22°C)70°F (21°C)64°F (18°C)54°F (12°C)45°F (7°C)40°F (4°C)
Rainfall4.9 in (124 mm)5.1 in (130 mm)5.6 in (141 mm)5 in (127 mm)4.1 in (104 mm)4.1 in (103 mm)4.1 in (103 mm)3.5 in (89 mm)3.2 in (81 mm)3.7 in (94 mm)3.9 in (98 mm)5.2 in (131 mm)
Rainy days101011101013141287810
Snowfall0.6 in (1.5 cm)0.3 in (0.7 cm)0.5 in (1.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)0.1 in (0.3 cm)
Sunshine204 h195 h263 h296 h346 h351 h367 h344 h302 h276 h228 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

+2.3°F (+1.3°C)

Models range from +1.8°F (+1.0°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

53 78

About 1.5× as many

Warming by month
  • January: +2.6°F (+1.4°C)
  • February: +3.1°F (+1.7°C)
  • March: +2.8°F (+1.5°C)
  • April: +2.0°F (+1.1°C)
  • May: +2.4°F (+1.3°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.9°F (+1.6°C)
  • September: +2.7°F (+1.5°C)
  • October: +3.1°F (+1.7°C)
  • November: +3.0°F (+1.7°C)
  • December: +2.5°F (+1.4°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.