ClimateSearch

Twifu Praso, Central

Ghana · 101k people · 73 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 high89°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)86°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)87°F (31°C)
Average low73°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)
Dew point71°F (22°C)73°F (23°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)71°F (22°C)72°F (22°C)73°F (23°C)74°F (23°C)73°F (23°C)
Rainfall2.1 in (52 mm)3.2 in (82 mm)5.4 in (136 mm)6 in (152 mm)8 in (204 mm)9 in (228 mm)5.9 in (150 mm)4.5 in (114 mm)7.2 in (183 mm)7.9 in (202 mm)4.9 in (125 mm)2.5 in (64 mm)
Rainy days121723252828242327292415
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)
Sunshine312 h280 h306 h301 h290 h250 h251 h226 h246 h290 h308 h313 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

+1.0°F (+0.6°C)

Models range from +0.3°F (+0.1°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

48 77

About 1.6× as many

Warming by month
  • January: +0.6°F (+0.4°C)
  • February: +1.0°F (+0.5°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.1°F (+0.6°C)
  • August: +0.5°F (+0.3°C)
  • September: +0.9°F (+0.5°C)
  • October: +1.0°F (+0.5°C)
  • November: +0.9°F (+0.5°C)
  • December: +0.5°F (+0.3°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.