ClimateSearch

Nong Chok, Bangkok

Thailand · 157k 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 high88°F (31°C)91°F (33°C)93°F (34°C)95°F (35°C)94°F (34°C)92°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)88°F (31°C)
Average low71°F (21°C)73°F (23°C)76°F (25°C)78°F (26°C)78°F (26°C)78°F (26°C)78°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)74°F (23°C)71°F (22°C)
Dew point65°F (19°C)68°F (20°C)72°F (22°C)74°F (24°C)76°F (24°C)76°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 (9 mm)0.5 in (13 mm)1.6 in (42 mm)3.2 in (81 mm)5.9 in (150 mm)4.9 in (125 mm)5.1 in (128 mm)6 in (152 mm)11 in (281 mm)7.3 in (185 mm)1.4 in (35 mm)0.4 in (10 mm)
Rainy days114512111114201431
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)
Sunshine239 h227 h240 h219 h172 h136 h124 h112 h118 h167 h206 h224 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 +1.2°F (+0.7°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

144 → 200

About 1.4× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.0°F (+0.6°C)
  • March: +1.0°F (+0.5°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.5°F (+0.8°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.