ClimateSearch

Santa Lucía Cotzumalguapa, Escuintla

Guatemala · 113k people · 387 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 high85°F (30°C)87°F (31°C)88°F (31°C)87°F (31°C)83°F (29°C)81°F (27°C)82°F (28°C)82°F (28°C)80°F (27°C)80°F (27°C)82°F (28°C)84°F (29°C)
Average low65°F (18°C)66°F (19°C)67°F (20°C)69°F (20°C)69°F (21°C)68°F (20°C)68°F (20°C)68°F (20°C)67°F (20°C)67°F (19°C)66°F (19°C)65°F (18°C)
Dew point61°F (16°C)61°F (16°C)63°F (17°C)66°F (19°C)69°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)69°F (21°C)67°F (19°C)64°F (18°C)
Rainfall0.3 in (8 mm)0.3 in (7 mm)0.8 in (20 mm)2.4 in (61 mm)9.7 in (247 mm)13.5 in (343 mm)9.9 in (252 mm)11.6 in (296 mm)14.9 in (379 mm)13.4 in (340 mm)3.9 in (99 mm)0.6 in (17 mm)
Rainy days32613262828292927155
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)
Sunshine337 h314 h359 h351 h322 h281 h321 h312 h274 h289 h315 h335 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 +1.8°F (+1.0°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

23 52

About 2.2× as many

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +1.7°F (+1.0°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.0°F (+1.1°C)
  • September: +1.8°F (+1.0°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.7°F (+1.0°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.