ClimateSearch

Piedecuesta, Santander Department

Colombia · 163k people · 1014 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 high77°F (25°C)78°F (25°C)78°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (25°C)
Average low63°F (17°C)64°F (18°C)64°F (18°C)65°F (18°C)65°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)64°F (18°C)63°F (17°C)
Dew point65°F (18°C)65°F (18°C)66°F (19°C)66°F (19°C)67°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)66°F (19°C)65°F (19°C)65°F (18°C)
Rainfall9.1 in (232 mm)10.3 in (261 mm)13 in (330 mm)17.1 in (433 mm)19.6 in (497 mm)17.8 in (451 mm)15.1 in (384 mm)12.4 in (316 mm)16.7 in (425 mm)21.5 in (547 mm)24.8 in (630 mm)18.9 in (481 mm)
Rainy days242227293028292828302927
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)
Sunshine338 h307 h326 h275 h259 h262 h290 h302 h276 h276 h271 h317 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: +1.7°F (+1.0°C)
  • February: +1.3°F (+0.7°C)
  • March: +1.5°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: +2.0°F (+1.1°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.