ClimateSearch

Phasi Charoen, Bangkok

Thailand · 122k people · 8 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 high88°F (31°C)90°F (32°C)92°F (34°C)94°F (35°C)92°F (33°C)90°F (32°C)89°F (32°C)89°F (31°C)88°F (31°C)87°F (30°C)87°F (31°C)87°F (31°C)
Average low72°F (22°C)75°F (24°C)78°F (26°C)81°F (27°C)80°F (27°C)79°F (26°C)78°F (26°C)78°F (26°C)77°F (25°C)76°F (24°C)74°F (23°C)72°F (22°C)
Dew point66°F (19°C)69°F (21°C)73°F (23°C)74°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)74°F (23°C)69°F (21°C)64°F (18°C)
Rainfall0.6 in (14 mm)0.6 in (15 mm)1.6 in (40 mm)2.7 in (70 mm)5.4 in (137 mm)5.3 in (134 mm)5.5 in (140 mm)5.9 in (150 mm)9.4 in (239 mm)7.8 in (198 mm)1.7 in (43 mm)0.4 in (10 mm)
Rainy days3371121222324262162
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)
Sunshine328 h305 h334 h334 h324 h291 h275 h259 h257 h292 h305 h317 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

+1.7°F (+0.9°C)

Models range from +1.5°F (+0.8°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

145 210

About 1.4× as many

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.2°F (+0.6°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.4°F (+1.4°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.5°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.5°F (+0.8°C)
  • December: +1.4°F (+0.8°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.