ClimateSearch

Kolda, Kolda

Senegal · 104k people · 13 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)102°F (39°C)103°F (39°C)100°F (38°C)95°F (35°C)88°F (31°C)87°F (30°C)88°F (31°C)91°F (33°C)93°F (34°C)93°F (34°C)
Average low60°F (16°C)64°F (18°C)68°F (20°C)72°F (22°C)74°F (23°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)73°F (23°C)67°F (19°C)60°F (16°C)
Dew point40°F (4°C)39°F (4°C)45°F (7°C)53°F (12°C)61°F (16°C)70°F (21°C)74°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)64°F (18°C)48°F (9°C)
Rainfall0 in (0 mm)0 in (1 mm)0 in (0 mm)0 in (0 mm)0.4 in (9 mm)3.1 in (79 mm)8.7 in (221 mm)11.1 in (282 mm)8 in (204 mm)2.6 in (65 mm)0.1 in (4 mm)0 in (1 mm)
Rainy days000016151915500
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)
Sunshine235 h230 h282 h276 h267 h210 h149 h121 h141 h203 h224 h224 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

+1.9°F (+1.0°C)

Models range from +1.3°F (+0.7°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

239 → 270

About 1.1× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.9°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +1.7°F (+1.0°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.9°F (+1.0°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.9°F (+1.0°C)
  • December: +1.7°F (+0.9°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.