ClimateSearch

Tarakan, North Kalimantan

Indonesia · 255k people · 27 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 high82°F (28°C)82°F (28°C)82°F (28°C)83°F (29°C)84°F (29°C)83°F (29°C)83°F (28°C)83°F (29°C)83°F (29°C)83°F (28°C)83°F (28°C)82°F (28°C)
Average low76°F (25°C)76°F (25°C)76°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)77°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)
Dew point74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)
Rainfall10.8 in (275 mm)8.2 in (208 mm)9.6 in (244 mm)9.7 in (247 mm)10.9 in (276 mm)9.4 in (238 mm)8.8 in (223 mm)8.8 in (223 mm)9.6 in (245 mm)11 in (280 mm)11.6 in (293 mm)12.2 in (310 mm)
Rainy days272529282927272728292930
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)
Sunshine287 h277 h310 h313 h320 h306 h316 h325 h316 h312 h300 h299 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

+0.8°F (+0.5°C)

Models range from −0.8°F (−0.5°C) to +1.4°F (+0.8°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +1.1°F (+0.6°C)
  • February: +0.7°F (+0.4°C)
  • March: +0.8°F (+0.4°C)
  • April: +1.0°F (+0.5°C)
  • May: +0.7°F (+0.4°C)
  • June: +0.8°F (+0.4°C)
  • July: +0.8°F (+0.4°C)
  • August: +0.9°F (+0.5°C)
  • September: +0.6°F (+0.3°C)
  • October: +0.6°F (+0.3°C)
  • November: +0.8°F (+0.5°C)
  • December: +0.8°F (+0.5°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.