ClimateSearch

Divo, Goh-Djiboua

Ivory Coast · 137k people · 145 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)93°F (34°C)92°F (33°C)91°F (33°C)89°F (32°C)85°F (30°C)84°F (29°C)83°F (29°C)85°F (30°C)87°F (31°C)89°F (31°C)89°F (32°C)
Average low71°F (21°C)73°F (23°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)72°F (22°C)72°F (22°C)73°F (23°C)72°F (22°C)
Dew point71°F (21°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)72°F (22°C)70°F (21°C)70°F (21°C)71°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)
Rainfall0.5 in (12 mm)2.2 in (56 mm)4 in (102 mm)4.5 in (114 mm)6.9 in (176 mm)9.6 in (244 mm)3.3 in (85 mm)2.1 in (53 mm)4.3 in (109 mm)4.7 in (120 mm)3.1 in (79 mm)1.4 in (37 mm)
Rainy days141011151784101273
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)
Sunshine201 h169 h173 h161 h149 h129 h126 h97 h122 h162 h183 h197 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

+1.4°F (+0.8°C)

Models range from +0.9°F (+0.5°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

55 → 90

About 1.6× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.9°F (+1.1°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.2°F (+0.7°C)
  • November: +1.2°F (+0.7°C)
  • December: +0.8°F (+0.4°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.