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 high88°F (31°C)89°F (32°C)90°F (32°C)91°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)87°F (31°C)
Average low74°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°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)
Rainfall9.9 in (253 mm)6.6 in (168 mm)11.4 in (289 mm)11.6 in (293 mm)9.2 in (233 mm)6.1 in (156 mm)5.3 in (134 mm)7.3 in (186 mm)8.8 in (224 mm)13.1 in (333 mm)16.1 in (408 mm)11.5 in (293 mm)
Rainy days141117201612111315202319
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)
Sunshine156 h165 h175 h156 h153 h159 h161 h157 h146 h136 h113 h123 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.