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 high91°F (33°C)92°F (33°C)92°F (33°C)92°F (33°C)92°F (34°C)91°F (33°C)91°F (33°C)92°F (33°C)93°F (34°C)92°F (33°C)92°F (33°C)92°F (33°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)76°F (25°C)76°F (25°C)76°F (25°C)76°F (25°C)77°F (25°C)77°F (25°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)
Rainfall8.4 in (212 mm)6.8 in (174 mm)9.8 in (248 mm)10 in (253 mm)7.5 in (190 mm)6.1 in (155 mm)4.9 in (126 mm)4.2 in (106 mm)4.8 in (121 mm)6.3 in (160 mm)8.6 in (219 mm)8.7 in (220 mm)
Rainy days191621211915131112152020
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)
Sunshine117 h116 h134 h131 h150 h150 h167 h189 h178 h153 h124 h114 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.