ClimateSearch

Tasek Glugor, Penang

Malaysia · 136k people · 6 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 high86°F (30°C)88°F (31°C)88°F (31°C)87°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)84°F (29°C)
Average low73°F (23°C)74°F (23°C)75°F (24°C)76°F (24°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)
Dew point72°F (22°C)72°F (22°C)74°F (23°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (23°C)73°F (23°C)
Rainfall4.9 in (124 mm)4.2 in (107 mm)7.5 in (190 mm)9.5 in (242 mm)9.8 in (250 mm)6.3 in (161 mm)6.4 in (161 mm)7.9 in (199 mm)10 in (253 mm)13.6 in (347 mm)13.1 in (332 mm)8.1 in (205 mm)
Rainy days161523282721212426292721
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)
Sunshine307 h294 h314 h300 h300 h293 h298 h291 h270 h257 h251 h273 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 +1.5°F (+0.8°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

17 37

About 2.2× as many

Warming by month
  • January: +0.8°F (+0.4°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.5°F (+0.8°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.5°F (+0.9°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.5°F (+0.9°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.7°F (+0.9°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.