ClimateSearch

Pattaya, Chon Buri

Thailand · 116k people · 6 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)90°F (32°C)91°F (33°C)93°F (34°C)93°F (34°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)91°F (33°C)89°F (32°C)
Average low72°F (22°C)75°F (24°C)78°F (25°C)80°F (27°C)80°F (27°C)80°F (26°C)79°F (26°C)79°F (26°C)77°F (25°C)75°F (24°C)74°F (24°C)71°F (22°C)
Dew point68°F (20°C)71°F (22°C)74°F (23°C)76°F (24°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)71°F (22°C)66°F (19°C)
Rainfall0.6 in (16 mm)0.7 in (17 mm)2.7 in (68 mm)4 in (101 mm)6.2 in (159 mm)4.2 in (107 mm)4 in (101 mm)4.8 in (123 mm)9.4 in (239 mm)10.1 in (256 mm)2.5 in (64 mm)0.6 in (16 mm)
Rainy days1158139911171851
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)
Sunshine235 h225 h239 h218 h166 h140 h133 h123 h117 h151 h200 h221 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

+1.2°F (+0.7°C)

Models range from +0.3°F (+0.2°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

56 → 89

About 1.6× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +0.9°F (+0.5°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.1°F (+0.6°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.3°F (+0.7°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.2°F (+0.7°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.