ClimateSearch

Izumisano, Osaka

Japan · 100k people · 5 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 high46°F (8°C)48°F (9°C)55°F (13°C)64°F (18°C)73°F (23°C)78°F (26°C)85°F (29°C)88°F (31°C)81°F (27°C)70°F (21°C)60°F (16°C)50°F (10°C)
Average low33°F (1°C)33°F (1°C)38°F (3°C)47°F (8°C)56°F (13°C)65°F (18°C)73°F (23°C)74°F (24°C)68°F (20°C)56°F (14°C)46°F (8°C)37°F (3°C)
Dew point31°F (-1°C)31°F (0°C)37°F (3°C)46°F (8°C)55°F (13°C)64°F (18°C)71°F (22°C)71°F (22°C)65°F (19°C)55°F (13°C)45°F (7°C)36°F (2°C)
Rainfall2.5 in (63 mm)2.8 in (70 mm)4.3 in (110 mm)4.5 in (114 mm)5.5 in (139 mm)7.8 in (198 mm)7.3 in (185 mm)4.3 in (108 mm)7.1 in (180 mm)6.7 in (169 mm)3.5 in (88 mm)2.8 in (71 mm)
Rainy days89121110141310131089
Snowfall0.7 in (1.7 cm)1.2 in (3.1 cm)0.1 in (0.2 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)0.3 in (0.7 cm)
Sunshine253 h240 h275 h275 h304 h260 h307 h337 h271 h258 h238 h248 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 +1.6°F (+0.9°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

15 32

About 2.2× as many

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.2°F (+1.2°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.