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 high86°F (30°C)86°F (30°C)88°F (31°C)89°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (31°C)88°F (31°C)88°F (31°C)87°F (31°C)
Average low74°F (24°C)74°F (24°C)75°F (24°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 (24°C)74°F (24°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)
Rainfall15.8 in (401 mm)9 in (228 mm)8.8 in (224 mm)8.8 in (223 mm)7.9 in (201 mm)9.7 in (246 mm)9.3 in (237 mm)9.5 in (241 mm)10.4 in (265 mm)13.4 in (339 mm)13.6 in (347 mm)17.6 in (447 mm)
Rainy days221617201717161720242526
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)
Sunshine114 h113 h135 h132 h139 h141 h149 h142 h131 h121 h112 h107 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.