ClimateSearch

Bandar Tasik Puteri, Selangor

Malaysia · 150k people · 48 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 high84°F (29°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)84°F (29°C)
Average low72°F (22°C)73°F (23°C)74°F (23°C)74°F (23°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)73°F (23°C)73°F (23°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)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)
Rainfall9.4 in (239 mm)6.7 in (171 mm)9.3 in (236 mm)10.6 in (269 mm)8.3 in (212 mm)5.1 in (129 mm)5.2 in (132 mm)5.7 in (144 mm)7.6 in (192 mm)10.3 in (262 mm)15.6 in (397 mm)12.6 in (321 mm)
Rainy days221824272318182021252726
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)
Sunshine296 h291 h316 h302 h305 h301 h306 h305 h291 h290 h257 h268 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 +0.8°F (+0.5°C) to +3.1°F (+1.7°C)

Days above 90°F (32°C) a year

8 15

About 1.9× as many

Warming by month
  • January: +0.8°F (+0.5°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.9°F (+1.0°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.4°F (+1.3°C)
  • November: +2.0°F (+1.1°C)
  • December: +1.7°F (+1.0°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.