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 high85°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)85°F (30°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)74°F (24°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (23°C)74°F (23°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)
Rainfall11 in (279 mm)9.6 in (243 mm)11.7 in (297 mm)12.2 in (309 mm)10.2 in (260 mm)9.2 in (233 mm)7.5 in (190 mm)6.6 in (169 mm)7 in (177 mm)8.9 in (227 mm)11.4 in (289 mm)12.6 in (320 mm)
Rainy days262327282926242121262829
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)
Sunshine278 h263 h295 h290 h307 h295 h310 h329 h322 h313 h285 h278 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.