ClimateSearch

Berbérati, Mambéré-Kadéï

Central African Republic · 104k people · 598 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 high89°F (32°C)91°F (33°C)90°F (32°C)88°F (31°C)87°F (31°C)84°F (29°C)83°F (28°C)83°F (28°C)84°F (29°C)85°F (29°C)87°F (30°C)88°F (31°C)
Average low63°F (17°C)65°F (19°C)68°F (20°C)68°F (20°C)68°F (20°C)67°F (19°C)67°F (19°C)67°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)64°F (18°C)
Dew point58°F (14°C)62°F (16°C)69°F (21°C)72°F (22°C)72°F (22°C)71°F (21°C)70°F (21°C)69°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)64°F (18°C)
Rainfall0.4 in (10 mm)0.8 in (20 mm)2.7 in (68 mm)4.6 in (118 mm)5.9 in (149 mm)5.7 in (144 mm)5.6 in (141 mm)6.9 in (175 mm)8.6 in (220 mm)8.1 in (205 mm)2.5 in (64 mm)0.4 in (10 mm)
Rainy days1261114141417192071
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)
Sunshine228 h189 h179 h163 h180 h168 h153 h136 h127 h132 h164 h222 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 +0.4°F (+0.2°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

69 → 81

About 1.2× as many

Warming by month
  • January: −0.3°F (−0.2°C)
  • February: +0.3°F (+0.2°C)
  • March: +0.8°F (+0.5°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.7°F (+0.9°C)
  • July: +0.9°F (+0.5°C)
  • August: +1.2°F (+0.6°C)
  • September: +1.0°F (+0.6°C)
  • October: +0.9°F (+0.5°C)
  • November: +1.0°F (+0.5°C)
  • December: +0.4°F (+0.2°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.