ClimateSearch

Touba, Diourbel Region

Senegal · 1.1M people · 44 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 high91°F (33°C)94°F (34°C)98°F (37°C)100°F (38°C)99°F (37°C)97°F (36°C)93°F (34°C)92°F (33°C)92°F (34°C)96°F (36°C)97°F (36°C)93°F (34°C)
Average low61°F (16°C)64°F (18°C)66°F (19°C)68°F (20°C)70°F (21°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)68°F (20°C)63°F (17°C)
Dew point34°F (1°C)35°F (2°C)40°F (4°C)49°F (9°C)56°F (13°C)65°F (19°C)70°F (21°C)73°F (23°C)74°F (23°C)68°F (20°C)49°F (10°C)40°F (4°C)
Rainfall0 in (1 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)1 in (26 mm)4 in (101 mm)5.5 in (140 mm)5.6 in (143 mm)1.3 in (33 mm)0 in (1 mm)0 in (1 mm)
Rainy days0000017109300
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)
Sunshine231 h225 h278 h280 h287 h257 h216 h170 h189 h240 h220 h215 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

+2.0°F (+1.1°C)

Models range from +1.8°F (+1.0°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

273 → 303

About 1.1× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.5°F (+0.8°C)
  • August: +2.1°F (+1.2°C)
  • September: +0.2°F (+0.1°C)
  • October: +0.4°F (+0.2°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.0°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.