ClimateSearch

Teshi Old Town, Greater Accra

Ghana · 144k people · 10 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 high87°F (31°C)88°F (31°C)88°F (31°C)88°F (31°C)85°F (30°C)82°F (28°C)80°F (27°C)80°F (26°C)81°F (27°C)83°F (28°C)85°F (30°C)87°F (31°C)
Average low76°F (25°C)78°F (26°C)79°F (26°C)78°F (26°C)78°F (25°C)76°F (24°C)74°F (23°C)73°F (23°C)74°F (24°C)75°F (24°C)77°F (25°C)77°F (25°C)
Dew point73°F (23°C)75°F (24°C)75°F (24°C)76°F (24°C)75°F (24°C)73°F (23°C)72°F (22°C)71°F (22°C)72°F (22°C)74°F (23°C)74°F (24°C)74°F (23°C)
Rainfall0.6 in (16 mm)0.8 in (22 mm)1.4 in (35 mm)1.9 in (49 mm)3.8 in (96 mm)5.5 in (141 mm)2 in (52 mm)1.4 in (36 mm)2.2 in (55 mm)2.4 in (62 mm)1.4 in (36 mm)0.8 in (21 mm)
Rainy days5691117201081313116
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)
Sunshine338 h303 h338 h332 h321 h281 h304 h301 h307 h329 h326 h338 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

+1.1°F (+0.6°C)

Models range from +0.6°F (+0.3°C) to +1.5°F (+0.8°C)

Days above 90°F (32°C) a year

9 21

About 2.2× as many

Warming by month
  • January: +0.8°F (+0.5°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.5°F (+0.9°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.0°F (+0.6°C)
  • August: +0.9°F (+0.5°C)
  • September: +1.0°F (+0.5°C)
  • October: +0.7°F (+0.4°C)
  • November: +0.8°F (+0.4°C)
  • December: +0.6°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.