ClimateSearch

Samarinda, East Kalimantan

Indonesia · 865k people · 20 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 high92°F (33°C)92°F (34°C)92°F (33°C)92°F (33°C)93°F (34°C)92°F (33°C)91°F (33°C)92°F (34°C)93°F (34°C)92°F (34°C)92°F (33°C)93°F (34°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 (24°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 (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)
Rainfall8 in (204 mm)6.7 in (169 mm)9.4 in (238 mm)9.8 in (248 mm)7.6 in (193 mm)6.4 in (163 mm)5.3 in (133 mm)4.2 in (108 mm)4.9 in (125 mm)6.3 in (160 mm)8.7 in (221 mm)8.7 in (221 mm)
Rainy days181620211815131112152020
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)
Sunshine124 h122 h143 h141 h159 h158 h173 h194 h184 h160 h131 h121 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

11 → 55

About 5.0× 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: +2.4°F (+1.4°C)
  • July: +2.6°F (+1.5°C)
  • August: +2.7°F (+1.5°C)
  • September: +2.4°F (+1.4°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.