ClimateSearch

Koforidua, Eastern

Ghana · 151k people · 171 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)91°F (33°C)89°F (32°C)87°F (30°C)83°F (28°C)82°F (28°C)82°F (28°C)83°F (28°C)84°F (29°C)86°F (30°C)88°F (31°C)
Average low73°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)72°F (22°C)71°F (22°C)71°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)
Dew point69°F (21°C)72°F (22°C)74°F (23°C)74°F (23°C)74°F (23°C)72°F (22°C)71°F (21°C)70°F (21°C)71°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)
Rainfall1.6 in (41 mm)2.3 in (58 mm)3.9 in (100 mm)4.5 in (113 mm)6.5 in (165 mm)7.6 in (192 mm)5 in (126 mm)4.1 in (105 mm)6.6 in (167 mm)6 in (152 mm)3.2 in (81 mm)1.6 in (42 mm)
Rainy days81219212526222126261810
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)
Sunshine330 h294 h325 h320 h306 h261 h268 h253 h267 h303 h315 h326 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

+1.2°F (+0.7°C)

Models range from +0.8°F (+0.5°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

78 114

About 1.5× as many

Warming by month
  • January: +0.7°F (+0.4°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.2°F (+0.7°C)
  • August: +0.6°F (+0.3°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.2°F (+0.6°C)
  • November: +1.1°F (+0.6°C)
  • December: +0.8°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.