ClimateSearch

Nkongsamba, Littoral

Cameroon · 162k people · 841 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 high82°F (28°C)83°F (29°C)81°F (27°C)80°F (26°C)78°F (26°C)76°F (25°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (25°C)78°F (26°C)80°F (27°C)
Average low65°F (19°C)67°F (19°C)68°F (20°C)68°F (20°C)67°F (20°C)67°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)
Dew point65°F (18°C)66°F (19°C)68°F (20°C)69°F (21°C)69°F (20°C)68°F (20°C)67°F (19°C)67°F (19°C)67°F (20°C)68°F (20°C)68°F (20°C)66°F (19°C)
Rainfall2.2 in (55 mm)3.9 in (100 mm)10.5 in (267 mm)12.9 in (327 mm)12.3 in (313 mm)12.6 in (319 mm)14.8 in (375 mm)16.4 in (416 mm)15.7 in (400 mm)15.7 in (400 mm)8.5 in (217 mm)2.4 in (60 mm)
Rainy days121527293030303130312714
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)
Sunshine331 h291 h280 h242 h253 h230 h224 h205 h206 h228 h279 h330 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

+1.5°F (+0.9°C)

Models range from +1.2°F (+0.7°C) to +1.7°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: +0.5°F (+0.3°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.3°F (+0.7°C)
  • December: +0.8°F (+0.5°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.