ClimateSearch

Banjaran, West Java

Indonesia · 165k people · 674 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 high79°F (26°C)79°F (26°C)80°F (27°C)81°F (27°C)81°F (27°C)81°F (27°C)82°F (28°C)83°F (28°C)84°F (29°C)83°F (29°C)81°F (27°C)80°F (27°C)
Average low68°F (20°C)69°F (20°C)69°F (20°C)69°F (20°C)68°F (20°C)67°F (20°C)67°F (19°C)67°F (19°C)68°F (20°C)69°F (21°C)69°F (21°C)69°F (20°C)
Dew point69°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)70°F (21°C)68°F (20°C)66°F (19°C)66°F (19°C)66°F (19°C)68°F (20°C)69°F (21°C)70°F (21°C)
Rainfall14.8 in (377 mm)14.1 in (358 mm)15.7 in (400 mm)12.9 in (329 mm)7.6 in (193 mm)5.5 in (139 mm)4.6 in (118 mm)3.9 in (100 mm)5.8 in (146 mm)12.7 in (323 mm)17.9 in (454 mm)16.6 in (422 mm)
Rainy days292729282318171517232729
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)
Sunshine237 h215 h258 h268 h313 h310 h336 h350 h327 h305 h246 h237 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 +1.7°F (+0.9°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

4 12

About 2.6× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +1.8°F (+1.0°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.8°F (+1.0°C)
  • August: +1.8°F (+1.0°C)
  • September: +2.0°F (+1.1°C)
  • October: +2.4°F (+1.3°C)
  • November: +1.8°F (+1.0°C)
  • December: +2.2°F (+1.2°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.