ClimateSearch

Man, Montagnes

Ivory Coast · 242k people · 333 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)92°F (33°C)90°F (32°C)88°F (31°C)87°F (30°C)84°F (29°C)81°F (27°C)81°F (27°C)82°F (28°C)83°F (29°C)85°F (29°C)88°F (31°C)
Average low70°F (21°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)
Dew point60°F (16°C)65°F (19°C)72°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)70°F (21°C)70°F (21°C)71°F (22°C)72°F (22°C)72°F (22°C)66°F (19°C)
Rainfall1 in (25 mm)2.3 in (58 mm)4.6 in (118 mm)4.8 in (122 mm)6 in (152 mm)6.7 in (169 mm)7.1 in (181 mm)8.5 in (215 mm)9.6 in (245 mm)5.8 in (147 mm)2.3 in (59 mm)0.8 in (21 mm)
Rainy days591921222525262825145
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 h294 h312 h296 h305 h279 h249 h223 h261 h307 h310 h327 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 (+0.8°C)

Models range from +1.2°F (+0.7°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

69 102

About 1.5× as many

Warming by month
  • January: +0.7°F (+0.4°C)
  • February: +1.7°F (+1.0°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.1°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.5°F (+0.9°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: +1.5°F (+0.8°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.