ClimateSearch

Buenaventura, Valle del Cauca Department

Colombia · 240k people · 19 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 high79°F (26°C)81°F (27°C)81°F (27°C)81°F (27°C)80°F (27°C)79°F (26°C)79°F (26°C)79°F (26°C)79°F (26°C)79°F (26°C)78°F (26°C)79°F (26°C)
Average low72°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)
Dew point73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)
Rainfall27.7 in (705 mm)17.8 in (453 mm)22.8 in (578 mm)32.3 in (820 mm)43.2 in (1098 mm)38.2 in (972 mm)37.1 in (942 mm)36.9 in (937 mm)45.5 in (1156 mm)48.2 in (1225 mm)42.1 in (1070 mm)33.1 in (842 mm)
Rainy days302830303129303130313031
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)
Sunshine207 h202 h205 h165 h152 h131 h139 h132 h120 h140 h144 h178 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

+1.8°F (+1.0°C)

Models range from +1.6°F (+0.9°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.3°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.