ClimateSearch

Kure, Hiroshima

Japan · 215k people · 85 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 high49°F (10°C)50°F (10°C)56°F (13°C)65°F (18°C)73°F (23°C)78°F (26°C)85°F (30°C)88°F (31°C)82°F (28°C)73°F (23°C)63°F (17°C)54°F (12°C)
Average low36°F (2°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (15°C)66°F (19°C)74°F (23°C)76°F (24°C)69°F (21°C)59°F (15°C)49°F (9°C)39°F (4°C)
Dew point31°F (0°C)32°F (0°C)38°F (3°C)47°F (8°C)56°F (13°C)64°F (18°C)72°F (22°C)73°F (23°C)66°F (19°C)55°F (13°C)45°F (7°C)36°F (2°C)
Rainfall2 in (52 mm)2.7 in (70 mm)4.8 in (123 mm)5.8 in (146 mm)6.7 in (169 mm)9.9 in (251 mm)10 in (255 mm)6.4 in (163 mm)7.9 in (202 mm)5.7 in (144 mm)3.2 in (81 mm)2.2 in (57 mm)
Rainy days579109101079766
Snowfall0.6 in (1.5 cm)0.9 in (2.3 cm)0.3 in (0.8 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)
Sunshine157 h155 h176 h181 h185 h128 h173 h217 h177 h186 h170 h166 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

+2.1°F (+1.2°C)

Models range from +1.6°F (+0.9°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.9°F (+1.0°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.0°F (+1.1°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.4°F (+1.4°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.