ClimateSearch

Cobán, Alta Verapaz

Guatemala · 212k people · 1327 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 high68°F (20°C)70°F (21°C)73°F (23°C)76°F (25°C)76°F (25°C)75°F (24°C)74°F (23°C)74°F (24°C)74°F (24°C)72°F (22°C)69°F (20°C)68°F (20°C)
Average low56°F (13°C)57°F (14°C)58°F (14°C)60°F (16°C)62°F (17°C)63°F (17°C)62°F (17°C)62°F (17°C)62°F (17°C)61°F (16°C)58°F (15°C)57°F (14°C)
Dew point58°F (14°C)58°F (15°C)59°F (15°C)61°F (16°C)63°F (17°C)64°F (18°C)63°F (17°C)64°F (18°C)64°F (18°C)62°F (17°C)60°F (15°C)58°F (15°C)
Rainfall7.2 in (182 mm)4.2 in (106 mm)4.9 in (125 mm)5.7 in (146 mm)10.1 in (257 mm)16.5 in (420 mm)11.4 in (288 mm)11.8 in (300 mm)16.4 in (416 mm)14.8 in (377 mm)11.6 in (293 mm)7.3 in (186 mm)
Rainy days181413162429292929272219
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)
Sunshine265 h277 h328 h337 h328 h289 h321 h329 h296 h280 h253 h262 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

+2.6°F (+1.5°C)

Models range from +1.8°F (+1.0°C) to +4.9°F (+2.7°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.9°F (+1.1°C)
  • February: +2.4°F (+1.4°C)
  • March: +2.6°F (+1.5°C)
  • April: +3.1°F (+1.7°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.4°F (+1.3°C)
  • July: +2.7°F (+1.5°C)
  • August: +2.8°F (+1.6°C)
  • September: +2.6°F (+1.4°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.6°F (+0.9°C)
  • December: +2.3°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.