ClimateSearch

Wangsa Maju, Kuala Lumpur

Malaysia · 216k people · 180 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 high83°F (29°C)85°F (30°C)85°F (30°C)85°F (30°C)85°F (29°C)85°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)84°F (29°C)83°F (28°C)83°F (28°C)
Average low71°F (21°C)71°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)71°F (22°C)
Dew point71°F (22°C)71°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)
Rainfall8.2 in (208 mm)6.6 in (167 mm)10.2 in (259 mm)11.8 in (299 mm)9.3 in (236 mm)6.9 in (175 mm)7.3 in (186 mm)8.6 in (217 mm)9.2 in (233 mm)11.7 in (297 mm)14.9 in (379 mm)11.1 in (283 mm)
Rainy days211725282723252625272826
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)
Sunshine293 h290 h311 h299 h302 h296 h302 h300 h287 h285 h249 h261 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 (+1.0°C)

Models range from +1.4°F (+0.8°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

4 10

About 2.6× as many

Warming by month
  • January: +1.2°F (+0.7°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.9°F (+1.0°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.9°F (+1.1°C)
  • September: +1.5°F (+0.9°C)
  • October: +2.1°F (+1.2°C)
  • November: +2.0°F (+1.1°C)
  • December: +1.8°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.