ClimateSearch

Sumbawanga, Rukwa

Tanzania · 304k people · 1823 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 high72°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)75°F (24°C)78°F (26°C)79°F (26°C)76°F (25°C)73°F (23°C)
Average low59°F (15°C)59°F (15°C)59°F (15°C)59°F (15°C)56°F (14°C)53°F (12°C)52°F (11°C)55°F (13°C)58°F (14°C)61°F (16°C)61°F (16°C)60°F (15°C)
Dew point60°F (16°C)60°F (16°C)60°F (16°C)59°F (15°C)54°F (12°C)47°F (9°C)45°F (7°C)45°F (7°C)46°F (8°C)50°F (10°C)55°F (13°C)59°F (15°C)
Rainfall11.1 in (283 mm)8.7 in (221 mm)10.2 in (258 mm)5.8 in (147 mm)1 in (27 mm)0.1 in (2 mm)0 in (1 mm)0.1 in (2 mm)0.3 in (8 mm)1.4 in (35 mm)5.1 in (130 mm)10.3 in (263 mm)
Rainy days282325185000151526
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)
Sunshine278 h266 h301 h321 h352 h343 h355 h360 h350 h355 h314 h293 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

+1.6°F (+0.9°C)

Models range from +1.2°F (+0.7°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.9°F (+1.1°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.7°F (+0.9°C)
  • September: +2.0°F (+1.1°C)
  • October: +2.3°F (+1.3°C)
  • November: +1.1°F (+0.6°C)
  • December: +1.9°F (+1.0°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.