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 high47°F (8°C)48°F (9°C)54°F (12°C)62°F (17°C)69°F (21°C)74°F (24°C)81°F (27°C)84°F (29°C)78°F (26°C)70°F (21°C)60°F (16°C)51°F (11°C)
Average low38°F (3°C)38°F (3°C)42°F (6°C)50°F (10°C)58°F (15°C)66°F (19°C)73°F (23°C)76°F (24°C)70°F (21°C)61°F (16°C)51°F (11°C)42°F (6°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 (51 mm)2.8 in (71 mm)4.6 in (116 mm)5.4 in (137 mm)6.1 in (154 mm)9.2 in (233 mm)9 in (228 mm)5 in (126 mm)6.5 in (166 mm)4.5 in (113 mm)2.8 in (71 mm)2.5 in (62 mm)
Rainy days6810101013131111877
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)
Sunshine235 h236 h270 h280 h301 h255 h303 h331 h275 h265 h244 h240 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.