ClimateSearch

Kajang, Selangor

Malaysia · 236k people · 34 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)91°F (33°C)92°F (33°C)92°F (33°C)92°F (33°C)92°F (33°C)91°F (33°C)91°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)89°F (32°C)
Average low74°F (24°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)
Dew point73°F (23°C)73°F (23°C)74°F (23°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)
Rainfall7.8 in (198 mm)5.4 in (136 mm)8.1 in (205 mm)10.6 in (270 mm)7.9 in (201 mm)6.1 in (155 mm)5.3 in (133 mm)6.4 in (163 mm)7.3 in (185 mm)11.1 in (281 mm)14.1 in (359 mm)10.2 in (258 mm)
Rainy days141015201712111416202319
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)
Sunshine155 h164 h173 h156 h153 h157 h162 h157 h149 h139 h112 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

+1.6°F (+0.9°C)

Models range from +1.4°F (+0.8°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

14 → 30

About 2.1× as many

Warming by month
  • January: +1.0°F (+0.6°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.8°F (+1.0°C)
  • September: +1.5°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.