ClimateSearch

Séguéla, Woroba

Ivory Coast · 104k people · 350 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)94°F (35°C)93°F (34°C)91°F (33°C)89°F (32°C)86°F (30°C)83°F (29°C)83°F (28°C)85°F (29°C)86°F (30°C)88°F (31°C)91°F (33°C)
Average low69°F (20°C)72°F (22°C)74°F (23°C)74°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)71°F (21°C)71°F (22°C)71°F (22°C)71°F (22°C)69°F (21°C)
Dew point54°F (12°C)61°F (16°C)69°F (21°C)72°F (22°C)72°F (22°C)71°F (22°C)69°F (21°C)69°F (21°C)71°F (22°C)71°F (22°C)70°F (21°C)62°F (16°C)
Rainfall0.7 in (18 mm)1.6 in (42 mm)4 in (101 mm)4.8 in (122 mm)5.6 in (143 mm)5.6 in (143 mm)6.3 in (159 mm)8.1 in (205 mm)9 in (229 mm)6 in (153 mm)2.6 in (66 mm)0.6 in (16 mm)
Rainy days371417192022242622113
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)
Sunshine336 h301 h322 h310 h322 h293 h270 h245 h273 h316 h320 h335 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

+1.7°F (+1.0°C)

Models range from +1.4°F (+0.8°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

146 193

About 1.3× as many

Warming by month
  • January: +0.6°F (+0.3°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.9°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.1°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.