ClimateSearch

Bontang, East Kalimantan

Indonesia · 195k 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)91°F (33°C)91°F (33°C)92°F (33°C)92°F (33°C)91°F (33°C)91°F (33°C)92°F (33°C)92°F (34°C)92°F (33°C)91°F (33°C)91°F (33°C)
Average low76°F (24°C)76°F (25°C)76°F (25°C)76°F (25°C)77°F (25°C)76°F (24°C)76°F (24°C)76°F (24°C)76°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)
Dew point75°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)
Rainfall7.2 in (183 mm)5.7 in (145 mm)10.5 in (266 mm)9 in (227 mm)8.3 in (210 mm)6.5 in (166 mm)4 in (101 mm)4.4 in (112 mm)5.3 in (135 mm)5.4 in (137 mm)8.1 in (206 mm)7.7 in (197 mm)
Rainy days171421201916111112141919
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)
Sunshine125 h124 h142 h138 h155 h152 h166 h189 h180 h155 h126 h118 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 +1.3°F (+0.7°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

1 → 3

About 3.6× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.5°F (+0.9°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.7°F (+1.0°C)
  • December: +1.9°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.