ClimateSearch

Quetzaltenango, Quetzaltenango

Guatemala · 181k people · 2359 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 high66°F (19°C)67°F (20°C)68°F (20°C)68°F (20°C)67°F (20°C)66°F (19°C)66°F (19°C)67°F (19°C)66°F (19°C)65°F (19°C)65°F (18°C)65°F (19°C)
Average low52°F (11°C)52°F (11°C)53°F (12°C)55°F (13°C)56°F (13°C)56°F (14°C)56°F (13°C)56°F (13°C)56°F (13°C)56°F (13°C)54°F (12°C)52°F (11°C)
Dew point48°F (9°C)48°F (9°C)51°F (10°C)54°F (12°C)56°F (14°C)57°F (14°C)55°F (13°C)55°F (13°C)57°F (14°C)56°F (13°C)53°F (11°C)50°F (10°C)
Rainfall1.3 in (32 mm)1.6 in (40 mm)4.2 in (106 mm)9.5 in (241 mm)20.1 in (511 mm)17.4 in (442 mm)11.3 in (287 mm)13.8 in (351 mm)18.5 in (469 mm)14.1 in (359 mm)4.6 in (117 mm)1.7 in (44 mm)
Rainy days101121273029282930292012
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 h311 h353 h344 h308 h267 h310 h304 h263 h276 h306 h327 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 +2.0°F (+1.1°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +2.0°F (+1.1°C)
  • March: +2.3°F (+1.3°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.1°F (+1.1°C)
  • October: +1.6°F (+0.9°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.1°F (+1.2°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.