ClimateSearch

Quibdó, Chocó

Colombia · 129k people · 33 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 high83°F (29°C)85°F (29°C)85°F (30°C)84°F (29°C)83°F (29°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)82°F (28°C)81°F (27°C)82°F (28°C)
Average low73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)
Dew point73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)
Rainfall15.6 in (395 mm)12.6 in (321 mm)18.4 in (469 mm)23.5 in (596 mm)29.8 in (757 mm)31 in (786 mm)28.9 in (734 mm)31.8 in (809 mm)29.4 in (747 mm)33.2 in (844 mm)32.5 in (825 mm)23.7 in (602 mm)
Rainy days272428293029303030302928
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)
Sunshine213 h196 h204 h167 h157 h138 h151 h153 h144 h156 h154 h179 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 +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

5 12

About 2.3× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.0°F (+0.5°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.5°F (+0.9°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.