ClimateSearch

Villa Nueva, Guatemala

Guatemala · 618k people · 1331 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 high79°F (26°C)82°F (28°C)84°F (29°C)84°F (29°C)82°F (28°C)80°F (26°C)81°F (27°C)81°F (27°C)80°F (27°C)79°F (26°C)79°F (26°C)80°F (27°C)
Average low57°F (14°C)57°F (14°C)58°F (15°C)60°F (16°C)62°F (17°C)62°F (17°C)62°F (16°C)62°F (17°C)62°F (16°C)61°F (16°C)58°F (15°C)57°F (14°C)
Dew point55°F (13°C)55°F (13°C)56°F (13°C)60°F (15°C)63°F (17°C)64°F (18°C)62°F (17°C)63°F (17°C)64°F (18°C)63°F (17°C)59°F (15°C)56°F (13°C)
Rainfall0 in (1 mm)0.1 in (4 mm)0.2 in (4 mm)1.3 in (34 mm)5.6 in (142 mm)11.6 in (295 mm)7.7 in (196 mm)7.8 in (197 mm)10.9 in (276 mm)5.6 in (143 mm)1 in (25 mm)0.1 in (3 mm)
Rainy days000415221517231430
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)
Sunshine250 h238 h262 h230 h166 h130 h176 h171 h132 h156 h205 h240 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

+2.2°F (+1.2°C)

Models range from +1.8°F (+1.0°C) to +3.1°F (+1.7°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 (+1.2°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.8°F (+1.5°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.0°F (+1.1°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.9°F (+1.1°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.