ClimateSearch

Kaolack, Kaolack

Senegal · 299k people · 3 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 high90°F (32°C)94°F (34°C)98°F (36°C)99°F (37°C)99°F (37°C)96°F (36°C)91°F (33°C)88°F (31°C)88°F (31°C)92°F (33°C)95°F (35°C)91°F (33°C)
Average low65°F (18°C)67°F (19°C)68°F (20°C)69°F (21°C)71°F (22°C)74°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)71°F (22°C)67°F (19°C)
Dew point38°F (3°C)38°F (3°C)43°F (6°C)51°F (11°C)59°F (15°C)68°F (20°C)72°F (22°C)74°F (23°C)75°F (24°C)72°F (22°C)56°F (13°C)44°F (7°C)
Rainfall0.1 in (2 mm)0 in (1 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.5 in (12 mm)3.5 in (88 mm)8 in (204 mm)5.9 in (151 mm)1.6 in (40 mm)0 in (1 mm)0.1 in (2 mm)
Rainy days000002112016600
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)
Sunshine322 h303 h353 h356 h365 h344 h319 h287 h298 h334 h317 h311 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 (+1.1°C)

Models range from +1.6°F (+0.9°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

258 291

About 1.1× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +2.2°F (+1.2°C)
  • March: +2.2°F (+1.2°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.9°F (+1.0°C)
  • September: +0.5°F (+0.3°C)
  • October: +1.0°F (+0.5°C)
  • November: +2.1°F (+1.2°C)
  • December: +1.9°F (+1.1°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.