ClimateSearch

Wang Thonglang, Bangkok

Thailand · 115k people · 5 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)92°F (33°C)93°F (34°C)95°F (35°C)95°F (35°C)94°F (34°C)92°F (33°C)92°F (33°C)92°F (33°C)91°F (33°C)92°F (33°C)91°F (33°C)
Average low72°F (22°C)74°F (24°C)77°F (25°C)79°F (26°C)79°F (26°C)79°F (26°C)78°F (26°C)78°F (26°C)77°F (25°C)76°F (25°C)75°F (24°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)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)69°F (21°C)64°F (18°C)
Rainfall0.4 in (11 mm)0.5 in (12 mm)1.5 in (38 mm)3 in (75 mm)6.8 in (174 mm)5.1 in (131 mm)5.8 in (148 mm)6.9 in (175 mm)11.7 in (297 mm)8.4 in (215 mm)1.4 in (36 mm)0.3 in (8 mm)
Rainy days113512111215191531
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)
Sunshine240 h230 h243 h222 h174 h136 h122 h111 h117 h164 h204 h223 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

+1.5°F (+0.8°C)

Models range from +0.7°F (+0.4°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

138 → 192

About 1.4× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +0.8°F (+0.5°C)
  • March: +0.8°F (+0.4°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.5°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.