ClimateSearch

Banjarmasin, South Kalimantan

Indonesia · 658k people · 5 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 (29°C)85°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)86°F (30°C)88°F (31°C)89°F (32°C)89°F (32°C)86°F (30°C)85°F (29°C)
Average low75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)76°F (24°C)75°F (24°C)74°F (23°C)74°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)
Dew point75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (23°C)73°F (23°C)71°F (22°C)72°F (22°C)73°F (23°C)75°F (24°C)75°F (24°C)
Rainfall12 in (304 mm)10.5 in (268 mm)11.4 in (290 mm)9.6 in (245 mm)6.3 in (160 mm)4.7 in (119 mm)3.7 in (93 mm)2.3 in (58 mm)3.1 in (78 mm)6.3 in (160 mm)10.3 in (262 mm)13.3 in (339 mm)
Rainy days292529282318151011192830
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)
Sunshine245 h231 h260 h262 h300 h292 h308 h320 h308 h298 h255 h231 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

+1.6°F (+0.9°C)

Models range from +1.4°F (+0.8°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

33 55

About 1.7× as many

Warming by month
  • January: +1.3°F (+0.7°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.6°F (+0.9°C)
  • May: +1.0°F (+0.6°C)
  • June: +1.2°F (+0.7°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.6°F (+0.9°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.5°F (+0.8°C)
  • November: +1.5°F (+0.9°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.