ClimateSearch

Prabumulih, South Sumatra

Indonesia · 103k people · 49 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 (31°C)88°F (31°C)89°F (32°C)88°F (31°C)88°F (31°C)89°F (32°C)91°F (33°C)90°F (32°C)88°F (31°C)87°F (30°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)74°F (23°C)73°F (23°C)73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)
Dew point74°F (23°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)71°F (22°C)71°F (22°C)72°F (22°C)74°F (23°C)74°F (23°C)
Rainfall13.4 in (342 mm)12.5 in (319 mm)14.2 in (360 mm)12.7 in (323 mm)8.3 in (210 mm)5.3 in (135 mm)4.5 in (115 mm)4.4 in (113 mm)3.6 in (92 mm)7.6 in (193 mm)12 in (305 mm)14.7 in (374 mm)
Rainy days2421242417121097152225
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)
Sunshine127 h119 h133 h140 h172 h183 h195 h201 h184 h157 h121 h108 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

+1.7°F (+1.0°C)

Models range from +1.5°F (+0.8°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

41 → 94

About 2.3× as many

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.7°F (+1.0°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.6°F (+1.4°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.3°F (+1.3°C)
  • December: +1.8°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.