ClimateSearch

Bouaflé, Sassandra-Marahoue

Ivory Coast · 104k people · 202 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 high94°F (34°C)96°F (35°C)94°F (35°C)92°F (34°C)91°F (33°C)87°F (31°C)85°F (29°C)85°F (29°C)86°F (30°C)88°F (31°C)90°F (32°C)91°F (33°C)
Average low67°F (20°C)71°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)71°F (21°C)70°F (21°C)71°F (22°C)71°F (22°C)70°F (21°C)68°F (20°C)
Dew point64°F (18°C)68°F (20°C)72°F (22°C)73°F (23°C)73°F (23°C)71°F (22°C)70°F (21°C)70°F (21°C)71°F (22°C)72°F (22°C)72°F (22°C)69°F (20°C)
Rainfall0.6 in (14 mm)1.8 in (46 mm)3.4 in (85 mm)4.2 in (107 mm)5.9 in (150 mm)6.1 in (155 mm)3.4 in (86 mm)4.3 in (109 mm)8 in (204 mm)4.7 in (118 mm)1.4 in (36 mm)0.6 in (15 mm)
Rainy days1479121279141031
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)
Sunshine227 h185 h182 h165 h162 h142 h120 h98 h129 h164 h179 h211 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

+1.3°F (+0.7°C)

Models range from +1.0°F (+0.6°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

114 → 148

About 1.3× as many

Warming by month
  • January: +0.6°F (+0.3°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.1°F (+0.6°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.1°F (+0.6°C)
  • November: +1.4°F (+0.8°C)
  • December: +0.9°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.