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 high88°F (31°C)88°F (31°C)89°F (31°C)89°F (32°C)89°F (32°C)89°F (32°C)88°F (31°C)88°F (31°C)89°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)
Average low74°F (23°C)74°F (23°C)74°F (23°C)75°F (24°C)74°F (23°C)72°F (22°C)71°F (21°C)71°F (21°C)72°F (22°C)74°F (23°C)74°F (24°C)74°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)
Rainfall12.2 in (310 mm)13.6 in (345 mm)11.5 in (292 mm)9.3 in (236 mm)4.9 in (125 mm)2.9 in (74 mm)1.5 in (38 mm)0.9 in (23 mm)1.2 in (32 mm)4.1 in (105 mm)9 in (227 mm)12.2 in (309 mm)
Rainy days232422199632281821
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)
Sunshine105 h95 h128 h146 h194 h198 h217 h226 h207 h194 h138 h110 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.