ClimateSearch

Mbandaka, Équateur

Democratic Republic of the Congo · 455k people · 313 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 high88°F (31°C)89°F (32°C)89°F (32°C)88°F (31°C)88°F (31°C)86°F (30°C)84°F (29°C)85°F (30°C)86°F (30°C)87°F (30°C)87°F (30°C)87°F (31°C)
Average low69°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)71°F (21°C)69°F (21°C)68°F (20°C)69°F (20°C)69°F (20°C)69°F (21°C)70°F (21°C)70°F (21°C)
Dew point73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)73°F (23°C)
Rainfall2.7 in (68 mm)3.4 in (85 mm)4.8 in (123 mm)5.5 in (139 mm)4.8 in (123 mm)3.4 in (88 mm)2.7 in (69 mm)5.2 in (132 mm)6.5 in (164 mm)8.2 in (208 mm)7 in (178 mm)3.8 in (98 mm)
Rainy days69111312961316191710
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)
Sunshine180 h153 h158 h149 h169 h179 h180 h164 h139 h132 h136 h162 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 (+0.7°C)

Models range from +0.6°F (+0.3°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

31 → 58

About 1.8× as many

Warming by month
  • January: +0.7°F (+0.4°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.2°F (+0.7°C)
  • August: +0.9°F (+0.5°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.0°F (+0.6°C)
  • November: +1.0°F (+0.5°C)
  • December: +0.7°F (+0.4°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.