ClimateSearch

Comitán, Chiapas

Mexico · 166k people · 1654 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 high78°F (25°C)80°F (27°C)83°F (29°C)85°F (30°C)84°F (29°C)80°F (27°C)80°F (27°C)80°F (27°C)80°F (27°C)78°F (26°C)78°F (25°C)77°F (25°C)
Average low51°F (10°C)52°F (11°C)53°F (12°C)56°F (14°C)59°F (15°C)61°F (16°C)60°F (15°C)60°F (16°C)60°F (16°C)58°F (15°C)54°F (12°C)51°F (11°C)
Dew point50°F (10°C)50°F (10°C)50°F (10°C)53°F (12°C)57°F (14°C)60°F (16°C)58°F (15°C)59°F (15°C)60°F (16°C)59°F (15°C)55°F (13°C)52°F (11°C)
Rainfall0.5 in (13 mm)0.4 in (11 mm)0.5 in (12 mm)1.4 in (35 mm)4.8 in (123 mm)9.8 in (248 mm)5.8 in (147 mm)7.8 in (198 mm)9.8 in (249 mm)5.6 in (143 mm)1.4 in (34 mm)0.7 in (17 mm)
Rainy days212412191215201342
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)
Sunshine256 h245 h278 h261 h211 h140 h190 h183 h143 h178 h215 h243 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 +1.9°F (+1.1°C) to +4.2°F (+2.3°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +2.2°F (+1.2°C)
  • March: +2.6°F (+1.4°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.5°F (+1.4°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.6°F (+1.5°C)
  • August: +2.7°F (+1.5°C)
  • September: +2.5°F (+1.4°C)
  • October: +1.8°F (+1.0°C)
  • November: +2.0°F (+1.1°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.