ClimateSearch

Higashiosaka, Osaka

Japan · 494k people · 6 m elevation · Northern 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 high47°F (8°C)49°F (9°C)55°F (13°C)65°F (18°C)74°F (23°C)80°F (26°C)86°F (30°C)89°F (32°C)82°F (28°C)71°F (22°C)61°F (16°C)51°F (11°C)
Average low34°F (1°C)34°F (1°C)38°F (4°C)47°F (9°C)57°F (14°C)65°F (19°C)73°F (23°C)76°F (24°C)69°F (20°C)57°F (14°C)47°F (8°C)38°F (3°C)
Dew point31°F (0°C)31°F (0°C)37°F (3°C)46°F (8°C)55°F (13°C)64°F (18°C)72°F (22°C)72°F (22°C)66°F (19°C)56°F (13°C)46°F (8°C)36°F (2°C)
Rainfall2.3 in (58 mm)2.6 in (67 mm)4.4 in (111 mm)4.7 in (118 mm)5.6 in (142 mm)7.6 in (194 mm)7.4 in (189 mm)4.2 in (107 mm)6.5 in (165 mm)6.2 in (158 mm)3.3 in (83 mm)2.5 in (63 mm)
Rainy days68111011131512121077
Snowfall0.4 in (1 cm)1.1 in (2.9 cm)0.1 in (0.3 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)0.2 in (0.4 cm)
Sunshine248 h233 h271 h271 h298 h258 h301 h334 h266 h253 h233 h242 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

+2.2°F (+1.2°C)

Models range from +1.7°F (+1.0°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

21 52

About 2.5× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.6°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.3°F (+1.3°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.