ClimateSearch

Situbondo, East Java

Indonesia · 686k people · 35 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 high83°F (28°C)83°F (28°C)83°F (29°C)84°F (29°C)86°F (30°C)86°F (30°C)87°F (31°C)88°F (31°C)90°F (32°C)90°F (32°C)87°F (30°C)84°F (29°C)
Average low74°F (24°C)74°F (24°C)74°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)73°F (23°C)72°F (22°C)74°F (23°C)75°F (24°C)75°F (24°C)75°F (24°C)
Dew point74°F (24°C)74°F (24°C)74°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)68°F (20°C)67°F (19°C)67°F (20°C)70°F (21°C)73°F (23°C)74°F (24°C)
Rainfall18.4 in (467 mm)15.5 in (394 mm)13.8 in (350 mm)9 in (229 mm)3 in (75 mm)1.5 in (38 mm)0.8 in (20 mm)0.2 in (5 mm)0.8 in (19 mm)2.6 in (67 mm)8.3 in (210 mm)16.8 in (427 mm)
Rainy days30272823138423102229
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)
Sunshine276 h258 h302 h303 h330 h321 h336 h342 h341 h360 h323 h289 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

+1.4°F (+0.8°C)

Models range from +0.8°F (+0.5°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

44 127

About 2.9× as many

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