ClimateSearch

Sampit, Central Kalimantan

Indonesia · 167k people · 4 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)87°F (30°C)86°F (30°C)87°F (30°C)86°F (30°C)86°F (30°C)87°F (31°C)88°F (31°C)88°F (31°C)87°F (30°C)86°F (30°C)
Average low74°F (24°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)74°F (23°C)74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)
Dew point74°F (24°C)74°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)74°F (24°C)73°F (23°C)72°F (22°C)73°F (23°C)74°F (23°C)75°F (24°C)75°F (24°C)
Rainfall10.5 in (267 mm)9.5 in (242 mm)11.7 in (297 mm)12.1 in (307 mm)8.3 in (212 mm)6.2 in (158 mm)4.7 in (119 mm)3.8 in (97 mm)5.4 in (136 mm)9.8 in (249 mm)12.5 in (317 mm)11.5 in (293 mm)
Rainy days282428292520171314222829
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)
Sunshine265 h245 h272 h265 h296 h291 h310 h317 h294 h280 h255 h253 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

+1.5°F (+0.9°C)

Models range from +1.5°F (+0.8°C) to +1.6°F (+0.9°C)

Days above 90°F (32°C) a year

18 31

About 1.7× as many

Warming by month
  • January: +1.5°F (+0.9°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.3°F (+0.7°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.2°F (+0.7°C)
  • November: +1.7°F (+0.9°C)
  • December: +1.6°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.