ClimateSearch

Daloa, Sassandra-Marahoue

Ivory Coast · 422k people · 261 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 high93°F (34°C)95°F (35°C)94°F (34°C)92°F (33°C)90°F (32°C)87°F (31°C)85°F (29°C)84°F (29°C)86°F (30°C)88°F (31°C)90°F (32°C)91°F (33°C)
Average low68°F (20°C)70°F (21°C)71°F (22°C)71°F (22°C)71°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)69°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)69°F (21°C)69°F (21°C)71°F (22°C)72°F (22°C)72°F (22°C)69°F (21°C)
Rainfall0.4 in (11 mm)2.2 in (56 mm)3.3 in (85 mm)3.8 in (97 mm)5.1 in (129 mm)5.6 in (143 mm)4 in (101 mm)6.3 in (159 mm)8.2 in (208 mm)4.9 in (125 mm)1.5 in (38 mm)0.6 in (15 mm)
Rainy days14791112811161231
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 h186 h176 h160 h158 h136 h113 h93 h127 h164 h172 h210 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

84 → 122

About 1.5× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.5°F (+0.8°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.3°F (+0.7°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.4°F (+0.8°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.