ClimateSearch

Coatepeque, Quetzaltenango

Guatemala · 105k people · 496 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 high82°F (28°C)84°F (29°C)85°F (29°C)84°F (29°C)82°F (28°C)80°F (27°C)80°F (27°C)80°F (27°C)79°F (26°C)79°F (26°C)80°F (26°C)81°F (27°C)
Average low64°F (18°C)65°F (18°C)66°F (19°C)68°F (20°C)69°F (20°C)68°F (20°C)67°F (20°C)68°F (20°C)68°F (20°C)67°F (19°C)66°F (19°C)64°F (18°C)
Dew point62°F (16°C)61°F (16°C)63°F (17°C)66°F (19°C)69°F (20°C)69°F (21°C)69°F (20°C)69°F (20°C)69°F (20°C)68°F (20°C)66°F (19°C)64°F (18°C)
Rainfall1 in (25 mm)0.8 in (21 mm)1.9 in (49 mm)5.5 in (139 mm)16.4 in (416 mm)19.9 in (505 mm)21.1 in (535 mm)23.3 in (591 mm)25.6 in (650 mm)24.1 in (612 mm)11 in (280 mm)2.2 in (55 mm)
Rainy days551118282829292928199
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)
Sunshine336 h309 h352 h352 h326 h272 h312 h301 h263 h282 h312 h329 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

+1.9°F (+1.0°C)

Models range from +1.6°F (+0.9°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

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