ClimateSearch

Pekalongan, Central Java

Indonesia · 325k people · 7 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)84°F (29°C)84°F (29°C)85°F (29°C)85°F (29°C)85°F (29°C)86°F (30°C)87°F (31°C)87°F (31°C)85°F (29°C)84°F (29°C)
Average low75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)73°F (23°C)74°F (24°C)76°F (24°C)76°F (24°C)75°F (24°C)
Dew point74°F (24°C)74°F (24°C)75°F (24°C)75°F (24°C)74°F (24°C)73°F (23°C)71°F (22°C)71°F (21°C)71°F (22°C)73°F (23°C)74°F (24°C)75°F (24°C)
Rainfall16.3 in (414 mm)15.4 in (390 mm)15.4 in (392 mm)13.8 in (350 mm)7.2 in (184 mm)5.3 in (134 mm)3.9 in (99 mm)2.9 in (74 mm)4.5 in (115 mm)10.8 in (274 mm)16.8 in (427 mm)19.6 in (497 mm)
Rainy days302830282216141114212729
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)
Sunshine260 h239 h287 h295 h323 h313 h339 h347 h328 h328 h286 h261 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 +1.3°F (+0.7°C) to +2.1°F (+1.1°C)

Days above 90°F (32°C) a year

16 53

About 3.4× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.5°F (+0.8°C)
  • March: +1.5°F (+0.9°C)
  • April: +1.7°F (+1.0°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.5°F (+0.8°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.4°F (+0.8°C)
  • November: +1.4°F (+0.8°C)
  • December: +1.9°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.