ClimateSearch

Lubumbashi, Haut-Katanga

Democratic Republic of the Congo · 2.2M people · 1261 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 high81°F (27°C)82°F (28°C)82°F (28°C)83°F (28°C)83°F (29°C)82°F (28°C)82°F (28°C)86°F (30°C)91°F (33°C)92°F (34°C)86°F (30°C)81°F (27°C)
Average low62°F (17°C)62°F (17°C)61°F (16°C)58°F (14°C)52°F (11°C)47°F (9°C)46°F (8°C)51°F (10°C)56°F (13°C)60°F (16°C)62°F (17°C)62°F (17°C)
Dew point64°F (18°C)64°F (18°C)64°F (18°C)59°F (15°C)51°F (11°C)45°F (7°C)42°F (6°C)42°F (5°C)43°F (6°C)50°F (10°C)61°F (16°C)64°F (18°C)
Rainfall9.8 in (249 mm)8.1 in (206 mm)7.4 in (188 mm)1.5 in (37 mm)0.1 in (3 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.1 in (3 mm)0.9 in (22 mm)5.2 in (133 mm)9.2 in (234 mm)
Rainy days23201951000141523
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)
Sunshine127 h124 h162 h218 h269 h277 h288 h293 h278 h251 h185 h137 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 +1.3°F (+0.7°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

22 → 33

About 1.5× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.4°F (+1.3°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.0°F (+1.1°C)
  • August: +1.8°F (+1.0°C)
  • September: +2.2°F (+1.2°C)
  • October: +2.8°F (+1.6°C)
  • November: +1.2°F (+0.7°C)
  • December: +1.5°F (+0.8°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.