ClimateSearch

Girón, Santander Department

Colombia · 108k people · 707 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 high86°F (30°C)86°F (30°C)86°F (30°C)85°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)87°F (30°C)87°F (30°C)85°F (30°C)84°F (29°C)85°F (29°C)
Average low68°F (20°C)69°F (20°C)70°F (21°C)69°F (21°C)69°F (21°C)69°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)
Dew point67°F (19°C)67°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)68°F (20°C)67°F (20°C)67°F (20°C)68°F (20°C)67°F (20°C)67°F (20°C)67°F (20°C)
Rainfall1.6 in (42 mm)2.5 in (63 mm)3.9 in (100 mm)7.7 in (195 mm)7.7 in (197 mm)5.4 in (138 mm)4.7 in (119 mm)5.3 in (135 mm)7.3 in (186 mm)10.9 in (276 mm)7.4 in (187 mm)3.8 in (96 mm)
Rainy days351018211614161823179
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)
Sunshine201 h180 h173 h122 h105 h110 h129 h138 h123 h122 h124 h172 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 +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.9°F (+1.0°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.6°F (+0.9°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.