ClimateSearch

Kennedy, Bogota D.C.

Colombia · 980k people · 2558 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 high66°F (19°C)67°F (19°C)66°F (19°C)65°F (18°C)65°F (18°C)65°F (18°C)65°F (18°C)67°F (20°C)68°F (20°C)66°F (19°C)65°F (19°C)66°F (19°C)
Average low51°F (11°C)52°F (11°C)52°F (11°C)53°F (11°C)53°F (11°C)52°F (11°C)52°F (11°C)52°F (11°C)51°F (11°C)51°F (11°C)51°F (11°C)51°F (11°C)
Dew point50°F (10°C)51°F (11°C)52°F (11°C)53°F (11°C)52°F (11°C)50°F (10°C)48°F (9°C)47°F (9°C)48°F (9°C)51°F (10°C)52°F (11°C)51°F (11°C)
Rainfall7.8 in (198 mm)8.5 in (216 mm)10 in (253 mm)9.6 in (244 mm)6.7 in (171 mm)2.1 in (54 mm)1.5 in (38 mm)1.3 in (32 mm)3.8 in (97 mm)8.7 in (221 mm)10.5 in (267 mm)8.6 in (218 mm)
Rainy days2122242319107614242623
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)
Sunshine332 h285 h289 h247 h252 h259 h281 h314 h308 h291 h277 h321 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

+2.1°F (+1.2°C)

Models range from +1.7°F (+1.0°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.5°F (+0.9°C)
  • March: +2.1°F (+1.1°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.5°F (+1.4°C)
  • November: +1.9°F (+1.0°C)
  • December: +2.1°F (+1.2°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.