ClimateSearch

Iwakuni, Yamaguchi

Japan · 129k people · 3 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 (9°C)49°F (10°C)55°F (13°C)64°F (18°C)72°F (22°C)77°F (25°C)84°F (29°C)86°F (30°C)80°F (27°C)71°F (22°C)61°F (16°C)51°F (11°C)
Average low37°F (3°C)37°F (3°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)70°F (21°C)60°F (15°C)50°F (10°C)41°F (5°C)
Dew point33°F (1°C)34°F (1°C)39°F (4°C)48°F (9°C)57°F (14°C)66°F (19°C)74°F (23°C)74°F (24°C)68°F (20°C)57°F (14°C)47°F (9°C)38°F (3°C)
Rainfall2 in (50 mm)2.8 in (70 mm)4.7 in (118 mm)5.5 in (139 mm)6.3 in (160 mm)9.4 in (240 mm)10.2 in (259 mm)6.7 in (171 mm)7.3 in (186 mm)4.5 in (115 mm)2.9 in (73 mm)2.4 in (62 mm)
Rainy days6810101014151412877
Snowfall1 in (2.6 cm)1.7 in (4.2 cm)0.7 in (1.7 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)0.4 in (1 cm)
Sunshine235 h236 h268 h278 h298 h251 h296 h326 h270 h264 h243 h239 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 (+1.1°C)

Models range from +1.7°F (+0.9°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

7 18

About 2.6× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.9°F (+1.0°C)
  • June: +1.8°F (+1.0°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.8°F (+1.6°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.