ClimateSearch

Bintulu, Sarawak

Malaysia · 152k people · 3 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 high84°F (29°C)85°F (29°C)86°F (30°C)87°F (30°C)87°F (31°C)87°F (31°C)87°F (31°C)87°F (31°C)87°F (30°C)86°F (30°C)85°F (30°C)85°F (29°C)
Average low74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)
Dew point74°F (24°C)74°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)
Rainfall13.5 in (342 mm)10.1 in (256 mm)9.4 in (239 mm)10.2 in (259 mm)10.2 in (258 mm)8.8 in (224 mm)8.3 in (210 mm)9.5 in (241 mm)10.4 in (264 mm)12.7 in (323 mm)13.7 in (347 mm)15.5 in (393 mm)
Rainy days272426272523222425292929
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)
Sunshine260 h248 h286 h279 h290 h284 h298 h292 h278 h273 h258 h255 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

+1.5°F (+0.8°C)

Models range from +1.4°F (+0.8°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

12 36

About 3.0× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.5°F (+0.9°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.4°F (+0.8°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.3°F (+0.7°C)
  • October: +1.5°F (+0.9°C)
  • November: +1.5°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.