ClimateSearch

Tuluá, Valle del Cauca Department

Colombia · 222k people · 979 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 high74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)74°F (23°C)
Average low60°F (16°C)61°F (16°C)62°F (17°C)62°F (17°C)61°F (16°C)60°F (16°C)60°F (16°C)60°F (16°C)60°F (16°C)61°F (16°C)62°F (17°C)61°F (16°C)
Dew point64°F (18°C)64°F (18°C)64°F (18°C)65°F (18°C)65°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)
Rainfall29.1 in (739 mm)29.4 in (747 mm)31.1 in (790 mm)36.8 in (936 mm)42.5 in (1080 mm)44 in (1117 mm)42.8 in (1088 mm)39.5 in (1003 mm)36.2 in (921 mm)32.5 in (824 mm)30.3 in (771 mm)30.7 in (780 mm)
Rainy days302730293130313029302930
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)
Sunshine290 h263 h264 h221 h221 h245 h270 h282 h250 h219 h205 h259 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

+1.6°F (+0.9°C)

Models range from +1.5°F (+0.8°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.9°F (+1.0°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.7°F (+1.0°C)
  • November: +1.3°F (+0.7°C)
  • December: +1.6°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.