ClimateSearch

Bégoua, Ombella-M'Poko

Central African Republic · 264k people · 405 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 high91°F (33°C)94°F (34°C)92°F (33°C)91°F (33°C)89°F (32°C)87°F (30°C)85°F (30°C)85°F (30°C)86°F (30°C)87°F (30°C)88°F (31°C)90°F (32°C)
Average low64°F (18°C)68°F (20°C)71°F (22°C)71°F (22°C)71°F (21°C)69°F (21°C)69°F (21°C)69°F (21°C)69°F (20°C)69°F (20°C)68°F (20°C)66°F (19°C)
Dew point58°F (14°C)62°F (17°C)71°F (21°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)65°F (18°C)
Rainfall0.3 in (8 mm)0.6 in (15 mm)2.5 in (63 mm)3.8 in (96 mm)5.2 in (133 mm)5.4 in (136 mm)6.9 in (175 mm)8.2 in (208 mm)7.1 in (180 mm)6.8 in (172 mm)2.3 in (59 mm)0.4 in (10 mm)
Rainy days126812121518181761
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)
Sunshine230 h196 h190 h177 h189 h181 h170 h147 h145 h144 h171 h218 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

+1.4°F (+0.8°C)

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

Days above 90°F (32°C) a year

116 → 139

About 1.2× as many

Warming by month
  • January: −0.5°F (−0.3°C)
  • February: +0.1°F (+0.1°C)
  • March: +1.2°F (+0.7°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.1°F (+0.6°C)
  • October: +0.9°F (+0.5°C)
  • November: +0.9°F (+0.5°C)
  • December: +0.1°F (+0.1°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.