ClimateSearch

Mbale, Eastern Region

Uganda · 111k people · 1121 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 high81°F (27°C)83°F (28°C)81°F (27°C)78°F (25°C)76°F (25°C)76°F (25°C)76°F (24°C)77°F (25°C)78°F (26°C)77°F (25°C)77°F (25°C)78°F (26°C)
Average low62°F (16°C)62°F (17°C)63°F (17°C)64°F (18°C)63°F (17°C)62°F (17°C)62°F (17°C)63°F (17°C)62°F (17°C)63°F (17°C)62°F (17°C)62°F (16°C)
Dew point59°F (15°C)59°F (15°C)62°F (16°C)64°F (18°C)64°F (18°C)62°F (17°C)61°F (16°C)62°F (16°C)62°F (17°C)62°F (17°C)62°F (17°C)61°F (16°C)
Rainfall14.8 in (377 mm)11.4 in (291 mm)24.5 in (623 mm)35.4 in (899 mm)31.8 in (807 mm)18.1 in (461 mm)9.6 in (243 mm)10.4 in (264 mm)17.9 in (455 mm)27.9 in (708 mm)33.6 in (854 mm)24.5 in (622 mm)
Rainy days232128303127242629312927
Snowfall0 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 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine346 h320 h328 h267 h290 h295 h302 h308 h308 h291 h276 h322 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

+1.7°F (+0.9°C)

Models range from +1.1°F (+0.6°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

4 6

About 1.7× as many

Warming by month
  • January: +0.8°F (+0.5°C)
  • February: +0.7°F (+0.4°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.9°F (+1.1°C)
  • May: +2.1°F (+1.1°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.0°F (+0.6°C)
  • October: +0.2°F (+0.1°C)
  • November: −0.1°F (−0.1°C)
  • December: +0.6°F (+0.3°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.