ClimateSearch

El Limón, Aragua

Venezuela · 148k people · 492 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 high80°F (27°C)81°F (27°C)82°F (28°C)82°F (28°C)83°F (28°C)82°F (28°C)81°F (27°C)82°F (28°C)83°F (28°C)83°F (28°C)81°F (27°C)80°F (27°C)
Average low69°F (20°C)69°F (20°C)70°F (21°C)72°F (22°C)73°F (23°C)72°F (22°C)71°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)70°F (21°C)
Dew point68°F (20°C)68°F (20°C)69°F (20°C)70°F (21°C)71°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)71°F (21°C)71°F (22°C)71°F (22°C)69°F (21°C)
Rainfall1.9 in (47 mm)1.7 in (43 mm)3.1 in (78 mm)6.5 in (165 mm)7.5 in (192 mm)6 in (152 mm)7.2 in (182 mm)5.8 in (146 mm)5.7 in (144 mm)7.2 in (183 mm)6.9 in (176 mm)3.5 in (89 mm)
Rainy days141315212525272624262520
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)
Sunshine333 h309 h334 h301 h310 h314 h330 h331 h313 h316 h298 h323 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

+2.0°F (+1.1°C)

Models range from +1.7°F (+1.0°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.1°F (+1.2°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.5°F (+0.8°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.