ClimateSearch

Mwanza, Mwanza

Tanzania · 1.1M people · 1142 m elevation · Southern 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 high82°F (28°C)83°F (29°C)84°F (29°C)83°F (28°C)83°F (28°C)83°F (28°C)82°F (28°C)83°F (28°C)83°F (29°C)83°F (29°C)82°F (28°C)82°F (28°C)
Average low66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)63°F (17°C)62°F (17°C)63°F (17°C)65°F (18°C)66°F (19°C)66°F (19°C)66°F (19°C)
Dew point65°F (19°C)65°F (19°C)65°F (19°C)65°F (19°C)63°F (17°C)59°F (15°C)56°F (14°C)59°F (15°C)62°F (17°C)64°F (18°C)65°F (19°C)65°F (19°C)
Rainfall3.4 in (87 mm)3 in (77 mm)4.2 in (107 mm)5.5 in (140 mm)2.2 in (57 mm)0.6 in (15 mm)0.3 in (9 mm)0.9 in (23 mm)1.2 in (30 mm)2.9 in (74 mm)5.5 in (139 mm)4.9 in (124 mm)
Rainy days11812137213391615
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)
Sunshine211 h196 h203 h175 h212 h227 h253 h246 h218 h181 h160 h197 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

+1.2°F (+0.6°C)

Models range from +0.8°F (+0.5°C) to +1.3°F (+0.7°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +2.0°F (+1.1°C)
  • May: +2.0°F (+1.1°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.0°F (+0.6°C)
  • November: +0.7°F (+0.4°C)
  • December: +1.2°F (+0.7°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.