ClimateSearch

Grogol, Central Java

Indonesia · 101k people · 92 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 high84°F (29°C)85°F (29°C)85°F (30°C)86°F (30°C)87°F (30°C)87°F (31°C)88°F (31°C)89°F (32°C)91°F (33°C)90°F (32°C)87°F (31°C)85°F (29°C)
Average low73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)71°F (22°C)71°F (21°C)72°F (22°C)73°F (23°C)74°F (23°C)73°F (23°C)
Dew point74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)71°F (22°C)69°F (20°C)67°F (20°C)68°F (20°C)71°F (22°C)73°F (23°C)74°F (23°C)
Rainfall14.1 in (358 mm)13.9 in (352 mm)13.1 in (332 mm)8.9 in (226 mm)4.3 in (110 mm)2.3 in (60 mm)1.5 in (38 mm)0.8 in (19 mm)1.6 in (41 mm)4.8 in (122 mm)9.6 in (243 mm)12.6 in (319 mm)
Rainy days282828251710746152527
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)
Sunshine250 h229 h273 h282 h318 h312 h333 h341 h325 h328 h280 h257 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

+2.0°F (+1.1°C)

Models range from +1.5°F (+0.9°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

61 110

About 1.8× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.0°F (+1.1°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.0°F (+1.1°C)
  • August: +2.0°F (+1.1°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.7°F (+1.5°C)
  • November: +1.7°F (+0.9°C)
  • December: +2.7°F (+1.5°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.