ClimateSearch

Valledupar, Cesar Department

Colombia · 490k people · 174 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 (29°C)83°F (28°C)82°F (28°C)83°F (28°C)84°F (29°C)85°F (29°C)83°F (28°C)81°F (27°C)80°F (27°C)82°F (28°C)
Average low68°F (20°C)69°F (21°C)70°F (21°C)71°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)70°F (21°C)69°F (21°C)
Dew point64°F (18°C)64°F (18°C)66°F (19°C)69°F (20°C)71°F (21°C)70°F (21°C)68°F (20°C)69°F (20°C)69°F (21°C)69°F (21°C)69°F (21°C)67°F (19°C)
Rainfall0.9 in (23 mm)1.4 in (35 mm)3.7 in (94 mm)9 in (230 mm)12.8 in (324 mm)6.1 in (154 mm)3.9 in (99 mm)5.7 in (145 mm)7.8 in (197 mm)12.1 in (308 mm)11.5 in (292 mm)3.4 in (87 mm)
Rainy days4612212823192225272211
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)
Sunshine344 h319 h342 h283 h258 h271 h296 h287 h262 h270 h280 h326 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 +1.5°F (+0.8°C) to +3.6°F (+2.0°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.1°C)
  • February: +1.8°F (+1.0°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.9°F (+1.1°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.8°F (+1.0°C)
  • December: +2.4°F (+1.3°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.