ClimateSearch

Si Racha, Chon Buri

Thailand · 179k people · 10 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 high86°F (30°C)87°F (31°C)88°F (31°C)89°F (32°C)88°F (31°C)87°F (31°C)86°F (30°C)86°F (30°C)85°F (30°C)85°F (30°C)86°F (30°C)86°F (30°C)
Average low74°F (23°C)76°F (24°C)78°F (26°C)80°F (27°C)80°F (27°C)80°F (27°C)80°F (26°C)79°F (26°C)78°F (26°C)77°F (25°C)76°F (24°C)73°F (23°C)
Dew point68°F (20°C)71°F (22°C)74°F (23°C)76°F (24°C)77°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)71°F (21°C)66°F (19°C)
Rainfall0.8 in (21 mm)0.9 in (23 mm)2.3 in (58 mm)3.5 in (89 mm)5.6 in (143 mm)5 in (126 mm)5.2 in (133 mm)5.3 in (135 mm)9.1 in (232 mm)7.8 in (198 mm)1.7 in (43 mm)0.4 in (11 mm)
Rainy days55111421212323252273
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)
Sunshine331 h306 h335 h333 h321 h298 h288 h275 h261 h290 h306 h322 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

+1.3°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

36 59

About 1.7× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.0°F (+0.6°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.5°F (+0.9°C)
  • June: +1.2°F (+0.6°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.3°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.