ClimateSearch

Puchong, Selangor

Malaysia · 375k people · 37 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)91°F (33°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)
Dew point73°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)
Rainfall8.7 in (220 mm)5.7 in (146 mm)8.9 in (225 mm)11 in (280 mm)8.2 in (208 mm)6.5 in (164 mm)5.1 in (130 mm)6.9 in (176 mm)7.8 in (199 mm)12.1 in (307 mm)14.5 in (369 mm)10.8 in (275 mm)
Rainy days141115191511101314192319
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)
Sunshine160 h168 h178 h161 h159 h164 h167 h162 h153 h144 h119 h128 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 +1.1°F (+0.6°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

11 → 22

About 2.0× as many

Warming by month
  • January: +0.9°F (+0.5°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.7°F (+0.9°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.2°F (+0.7°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.5°F (+0.9°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.