ClimateSearch

San Cristóbal, Táchira

Venezuela · 290k people · 815 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)82°F (28°C)81°F (27°C)81°F (27°C)82°F (28°C)83°F (29°C)83°F (28°C)81°F (27°C)80°F (27°C)
Average low63°F (17°C)64°F (18°C)65°F (19°C)65°F (19°C)66°F (19°C)66°F (19°C)65°F (18°C)65°F (19°C)65°F (18°C)65°F (19°C)65°F (18°C)64°F (18°C)
Dew point62°F (17°C)62°F (17°C)64°F (18°C)66°F (19°C)66°F (19°C)65°F (19°C)65°F (18°C)65°F (18°C)65°F (19°C)66°F (19°C)66°F (19°C)64°F (18°C)
Rainfall2.1 in (54 mm)1.8 in (46 mm)3.6 in (90 mm)5.9 in (150 mm)7.6 in (192 mm)12.2 in (310 mm)10.2 in (260 mm)7 in (178 mm)6 in (153 mm)8.4 in (214 mm)6.8 in (174 mm)4.2 in (108 mm)
Rainy days54710121414111113118
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)
Sunshine215 h187 h178 h127 h115 h123 h139 h151 h143 h140 h147 h194 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

+2.3°F (+1.3°C)

Models range from +1.4°F (+0.8°C) to +4.2°F (+2.4°C)

Days above 90°F (32°C) a year

1 → 4

About 6.1× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.9°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.0°F (+1.1°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.3°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.