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 high90°F (32°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)88°F (31°C)89°F (32°C)89°F (32°C)88°F (31°C)87°F (31°C)88°F (31°C)89°F (32°C)
Average low66°F (19°C)68°F (20°C)69°F (20°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)71°F (22°C)70°F (21°C)69°F (21°C)67°F (20°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)
Rainfall0.6 in (16 mm)1.2 in (29 mm)1.7 in (43 mm)5.1 in (129 mm)16.5 in (418 mm)23.9 in (607 mm)15 in (382 mm)16.9 in (429 mm)24 in (609 mm)21.1 in (536 mm)6.8 in (172 mm)1.3 in (34 mm)
Rainy days23510222723252824113
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)
Sunshine277 h258 h280 h250 h186 h135 h174 h164 h131 h161 h221 h268 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.