ClimateSearch

Tokuyama, Yamaguchi

Japan · 101k people · 36 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)51°F (10°C)56°F (14°C)65°F (18°C)73°F (23°C)78°F (26°C)85°F (29°C)88°F (31°C)82°F (28°C)73°F (23°C)64°F (18°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 (20°C)58°F (15°C)48°F (9°C)39°F (4°C)
Dew point33°F (0°C)33°F (1°C)39°F (4°C)47°F (9°C)57°F (14°C)66°F (19°C)74°F (23°C)74°F (24°C)67°F (20°C)56°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.2 in (55 mm)2.8 in (72 mm)4.8 in (122 mm)6.9 in (176 mm)7.6 in (193 mm)10.5 in (266 mm)12.3 in (311 mm)5 in (128 mm)7.8 in (198 mm)4.7 in (118 mm)3 in (77 mm)2.6 in (67 mm)
Rainy days8810119111289778
Snowfall2.6 in (6.6 cm)2.9 in (7.3 cm)1.1 in (2.7 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)1.3 in (3.4 cm)
Sunshine142 h146 h168 h177 h178 h121 h154 h199 h167 h185 h167 h156 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 +1.7°F (+0.9°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

7 → 18

About 2.7× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.9°F (+1.0°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.4°F (+1.3°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.