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 high88°F (31°C)88°F (31°C)89°F (32°C)89°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)
Average low74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)74°F (24°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)
Rainfall11.2 in (284 mm)8.4 in (213 mm)12.7 in (322 mm)11.4 in (291 mm)11.4 in (291 mm)11.4 in (289 mm)11.1 in (283 mm)10.9 in (277 mm)11 in (279 mm)13 in (331 mm)13.3 in (338 mm)14 in (355 mm)
Rainy days201621212221212121232425
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)
Sunshine144 h145 h173 h181 h179 h169 h175 h186 h179 h166 h158 h149 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.