ClimateSearch

Ébolowa, South

Cameroon · 101k people · 579 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 high84°F (29°C)85°F (29°C)84°F (29°C)84°F (29°C)83°F (28°C)82°F (28°C)80°F (27°C)80°F (27°C)81°F (27°C)81°F (27°C)82°F (28°C)83°F (28°C)
Average low70°F (21°C)70°F (21°C)71°F (21°C)70°F (21°C)70°F (21°C)69°F (21°C)68°F (20°C)68°F (20°C)69°F (21°C)69°F (21°C)69°F (21°C)70°F (21°C)
Dew point69°F (21°C)70°F (21°C)71°F (22°C)71°F (22°C)71°F (22°C)69°F (21°C)68°F (20°C)68°F (20°C)69°F (20°C)69°F (21°C)70°F (21°C)69°F (21°C)
Rainfall2.8 in (70 mm)3.6 in (91 mm)7.1 in (181 mm)8.1 in (205 mm)7.9 in (200 mm)7.4 in (187 mm)6.5 in (165 mm)6.1 in (156 mm)9.5 in (242 mm)11.2 in (284 mm)8 in (203 mm)3.5 in (90 mm)
Rainy days141625262726252628302515
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)
Sunshine287 h256 h267 h252 h266 h248 h231 h222 h228 h236 h243 h279 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 +1.0°F (+0.5°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +0.8°F (+0.4°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.0°F (+0.6°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.