ClimateSearch

George Town, Penang

Malaysia · 158k people · 7 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 high91°F (33°C)92°F (33°C)92°F (33°C)91°F (33°C)91°F (33°C)90°F (32°C)90°F (32°C)89°F (32°C)89°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)
Average low75°F (24°C)75°F (24°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)75°F (24°C)75°F (24°C)
Dew point73°F (23°C)73°F (23°C)75°F (24°C)76°F (25°C)76°F (25°C)76°F (25°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)
Rainfall6.1 in (155 mm)3.5 in (89 mm)6.8 in (173 mm)9.1 in (231 mm)9.4 in (239 mm)7.3 in (186 mm)7.8 in (197 mm)9.4 in (239 mm)11.9 in (303 mm)16.8 in (427 mm)13.3 in (337 mm)8.5 in (215 mm)
Rainy days10713181814141720252315
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)
Sunshine178 h179 h183 h160 h146 h148 h148 h141 h126 h113 h116 h137 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 +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

4 → 10

About 2.5× as many

Warming by month
  • January: +0.8°F (+0.5°C)
  • February: +1.1°F (+0.6°C)
  • March: +1.3°F (+0.7°C)
  • April: +1.5°F (+0.9°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.5°F (+0.8°C)
  • October: +1.8°F (+1.0°C)
  • November: +1.6°F (+0.9°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.