ClimateSearch

Kara, Kara

Togo · 104k people · 291 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 high94°F (35°C)98°F (37°C)98°F (37°C)96°F (35°C)91°F (33°C)87°F (31°C)83°F (29°C)82°F (28°C)84°F (29°C)87°F (31°C)92°F (33°C)94°F (34°C)
Average low66°F (19°C)70°F (21°C)74°F (24°C)76°F (25°C)75°F (24°C)73°F (23°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)68°F (20°C)66°F (19°C)
Dew point42°F (6°C)45°F (7°C)61°F (16°C)71°F (22°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)73°F (23°C)72°F (22°C)63°F (17°C)48°F (9°C)
Rainfall0.1 in (2 mm)0.4 in (9 mm)1.2 in (31 mm)3.4 in (87 mm)5.5 in (141 mm)6.2 in (157 mm)8.8 in (223 mm)11.6 in (294 mm)10.4 in (263 mm)5.3 in (135 mm)0.5 in (13 mm)0.1 in (1 mm)
Rainy days0251521232829271920
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)
Sunshine344 h315 h344 h324 h323 h293 h270 h247 h266 h314 h326 h340 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

+1.3°F (+0.7°C)

Models range from +0.7°F (+0.4°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

198 216

About 1.1× as many

Warming by month
  • January: −0.1°F (+0.0°C)
  • February: +0.6°F (+0.4°C)
  • March: +1.3°F (+0.7°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.0°F (+0.5°C)
  • September: +0.9°F (+0.5°C)
  • October: +0.5°F (+0.3°C)
  • November: +0.7°F (+0.4°C)
  • December: +0.0°F (+0.0°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.