ClimateSearch

Nishinomiya, Hyōgo

Japan · 486k people · 9 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)73°F (23°C)79°F (26°C)85°F (30°C)88°F (31°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)39°F (4°C)48°F (9°C)58°F (14°C)66°F (19°C)74°F (23°C)76°F (25°C)69°F (21°C)58°F (15°C)48°F (9°C)39°F (4°C)
Dew point32°F (0°C)33°F (0°C)38°F (3°C)47°F (8°C)56°F (14°C)65°F (18°C)73°F (23°C)74°F (23°C)67°F (19°C)57°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.2 in (56 mm)2.6 in (67 mm)4.4 in (112 mm)5 in (127 mm)5.9 in (151 mm)7.9 in (200 mm)8.2 in (209 mm)5.1 in (131 mm)7.5 in (192 mm)6.5 in (165 mm)3.4 in (86 mm)2.6 in (67 mm)
Rainy days67111011141514131077
Snowfall0.4 in (1.1 cm)1.3 in (3.2 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 (0.5 cm)
Sunshine246 h234 h271 h270 h299 h258 h299 h332 h266 h254 h233 h241 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 +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

16 43

About 2.7× 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: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.7°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.