ClimateSearch

Nusantara, East Kalimantan

Indonesia · 147k people · 37 m elevation · Southern 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 high89°F (32°C)90°F (32°C)90°F (32°C)90°F (32°C)91°F (33°C)90°F (32°C)89°F (32°C)90°F (32°C)91°F (33°C)91°F (33°C)90°F (32°C)91°F (33°C)
Average low75°F (24°C)75°F (24°C)76°F (24°C)76°F (25°C)76°F (25°C)76°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)76°F (24°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 (23°C)74°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)
Rainfall10.4 in (263 mm)8.7 in (221 mm)11.5 in (291 mm)11 in (279 mm)8.4 in (212 mm)7 in (178 mm)5.5 in (140 mm)5.5 in (139 mm)5 in (128 mm)6.7 in (170 mm)8.7 in (222 mm)9.8 in (250 mm)
Rainy days211922222016131211152022
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)
Sunshine111 h108 h125 h123 h146 h148 h165 h184 h174 h150 h115 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

+1.7°F (+1.0°C)

Models range from +1.5°F (+0.8°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

7 → 19

About 2.5× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.5°F (+0.8°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.7°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.