ClimateSearch

Loa Janan, East Kalimantan

Indonesia · 213k people · 8 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 high86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)85°F (30°C)85°F (29°C)86°F (30°C)87°F (31°C)87°F (31°C)86°F (30°C)86°F (30°C)
Average low74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)
Dew point75°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)76°F (25°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)
Rainfall10.7 in (271 mm)9.5 in (241 mm)11.7 in (297 mm)11.9 in (303 mm)10.1 in (256 mm)8.7 in (221 mm)7.2 in (183 mm)6.5 in (164 mm)6.5 in (165 mm)8.9 in (227 mm)11.3 in (287 mm)11.9 in (301 mm)
Rainy days272427282926242221262929
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)
Sunshine270 h255 h286 h280 h299 h288 h304 h325 h316 h307 h275 h269 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

+2.6°F (+1.4°C)

Models range from +1.3°F (+0.7°C) to +5.9°F (+3.3°C)

Days above 90°F (32°C) a year

12 56

About 4.8× as many

Warming by month
  • January: +2.6°F (+1.5°C)
  • February: +2.5°F (+1.4°C)
  • March: +2.6°F (+1.4°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.6°F (+1.4°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.6°F (+1.5°C)
  • August: +2.7°F (+1.5°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.9°F (+1.6°C)
  • December: +2.7°F (+1.5°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.