ClimateSearch

San, Ségou

Mali · 103k people · 283 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)96°F (36°C)102°F (39°C)104°F (40°C)103°F (40°C)98°F (37°C)92°F (33°C)88°F (31°C)90°F (32°C)94°F (34°C)94°F (35°C)91°F (33°C)
Average low56°F (13°C)61°F (16°C)68°F (20°C)74°F (23°C)78°F (25°C)75°F (24°C)73°F (23°C)72°F (22°C)73°F (23°C)73°F (23°C)66°F (19°C)58°F (15°C)
Dew point28°F (-2°C)26°F (-4°C)30°F (-1°C)47°F (8°C)62°F (17°C)69°F (20°C)71°F (22°C)72°F (22°C)73°F (23°C)65°F (18°C)42°F (6°C)33°F (1°C)
Rainfall0 in (1 mm)0 in (0 mm)0 in (1 mm)0.3 in (9 mm)1 in (27 mm)2.4 in (60 mm)5.4 in (136 mm)8.6 in (218 mm)4.2 in (106 mm)0.8 in (21 mm)0 in (0 mm)0 in (0 mm)
Rainy days00023511159200
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)
Sunshine257 h244 h254 h237 h238 h246 h214 h174 h207 h246 h245 h255 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

+1.5°F (+0.8°C)

Models range from +0.5°F (+0.3°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

279 → 297

About 1.1× as many

Warming by month
  • January: +0.8°F (+0.4°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.5°F (+1.4°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.3°F (+0.7°C)
  • September: +0.3°F (+0.2°C)
  • October: +0.6°F (+0.3°C)
  • November: +1.2°F (+0.6°C)
  • December: +1.2°F (+0.7°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.