ClimateSearch

Pangkalanbuun, Central Kalimantan

Indonesia · 109k people · 13 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 high88°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)90°F (32°C)89°F (32°C)89°F (32°C)89°F (32°C)90°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)74°F (24°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)
Dew point74°F (24°C)74°F (24°C)75°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)73°F (23°C)73°F (23°C)73°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)
Rainfall9.5 in (240 mm)9.8 in (249 mm)10.9 in (277 mm)11.6 in (296 mm)10 in (253 mm)7.9 in (200 mm)6.5 in (166 mm)5.1 in (131 mm)5.3 in (136 mm)8.4 in (212 mm)12.3 in (312 mm)11.8 in (301 mm)
Rainy days21182224191412910172424
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)
Sunshine114 h111 h128 h120 h158 h172 h190 h196 h166 h131 h104 h96 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

+1.8°F (+1.0°C)

Models range from +1.4°F (+0.8°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

9 → 24

About 2.7× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +2.0°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.1°F (+1.1°C)
  • May: +1.7°F (+1.0°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.1°F (+1.1°C)
  • September: +1.7°F (+1.0°C)
  • October: +1.8°F (+1.0°C)
  • November: +2.0°F (+1.1°C)
  • December: +1.9°F (+1.0°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.