ClimateSearch

Teziutlan, Puebla

Mexico · 104k people · 1934 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 high65°F (18°C)68°F (20°C)72°F (22°C)76°F (24°C)76°F (25°C)74°F (23°C)72°F (22°C)72°F (22°C)71°F (22°C)70°F (21°C)67°F (20°C)66°F (19°C)
Average low41°F (5°C)44°F (7°C)47°F (8°C)51°F (10°C)53°F (12°C)54°F (12°C)54°F (12°C)53°F (12°C)54°F (12°C)50°F (10°C)46°F (8°C)43°F (6°C)
Dew point47°F (8°C)49°F (9°C)51°F (10°C)54°F (12°C)56°F (14°C)58°F (14°C)57°F (14°C)57°F (14°C)57°F (14°C)55°F (13°C)51°F (11°C)49°F (9°C)
Rainfall1.2 in (31 mm)1 in (25 mm)1.3 in (33 mm)1.5 in (39 mm)2.3 in (58 mm)6.2 in (158 mm)5 in (127 mm)5.7 in (145 mm)8.7 in (221 mm)5.7 in (145 mm)2.5 in (62 mm)1.1 in (27 mm)
Rainy days667792020212315106
Snowfall0 in (0 cm)0 in (0 cm)0 in (0.1 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 (0.1 cm)
Sunshine181 h181 h208 h216 h234 h187 h201 h193 h144 h168 h169 h187 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

+2.4°F (+1.4°C)

Models range from +2.0°F (+1.1°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.6°F (+1.4°C)
  • August: +2.6°F (+1.4°C)
  • September: +2.4°F (+1.4°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.8°F (+1.0°C)
  • December: +2.6°F (+1.5°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.