ClimateSearch

Manizales, Caldas Department

Colombia · 434k people · 2123 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 high71°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)70°F (21°C)71°F (21°C)71°F (22°C)71°F (22°C)71°F (22°C)69°F (21°C)69°F (20°C)70°F (21°C)
Average low54°F (12°C)55°F (13°C)55°F (13°C)55°F (13°C)55°F (13°C)55°F (13°C)54°F (12°C)54°F (12°C)54°F (12°C)53°F (12°C)54°F (12°C)54°F (12°C)
Dew point54°F (12°C)54°F (12°C)55°F (13°C)56°F (13°C)56°F (13°C)55°F (13°C)55°F (13°C)54°F (12°C)55°F (13°C)55°F (13°C)55°F (13°C)55°F (13°C)
Rainfall5.2 in (133 mm)5.7 in (145 mm)7.9 in (202 mm)10.7 in (271 mm)10.3 in (261 mm)5.1 in (129 mm)3.8 in (96 mm)4.6 in (118 mm)6.7 in (170 mm)12.1 in (308 mm)10 in (253 mm)7.6 in (193 mm)
Rainy days232225272926252727282526
Snowfall0 in (0 cm)0 in (0.1 cm)0.1 in (0.3 cm)0.1 in (0.2 cm)0 in (0.1 cm)0 in (0.1 cm)0.1 in (0.2 cm)0.2 in (0.4 cm)0.4 in (0.9 cm)0.1 in (0.3 cm)0 in (0 cm)0 in (0 cm)
Sunshine167 h141 h132 h96 h96 h119 h141 h153 h130 h111 h106 h143 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

+1.9°F (+1.1°C)

Models range from +1.5°F (+0.8°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.1°F (+1.2°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.7°F (+0.9°C)
  • October: +1.7°F (+1.0°C)
  • November: +1.8°F (+1.0°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.