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 high47°F (9°C)49°F (10°C)56°F (13°C)64°F (18°C)72°F (22°C)78°F (25°C)84°F (29°C)86°F (30°C)80°F (27°C)72°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)69°F (21°C)59°F (15°C)50°F (10°C)41°F (5°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)
Rainfall2.4 in (61 mm)3.1 in (79 mm)5.1 in (129 mm)5.9 in (149 mm)6.7 in (171 mm)10.7 in (272 mm)12.1 in (308 mm)7.6 in (194 mm)7.9 in (200 mm)4.4 in (112 mm)3.2 in (81 mm)2.7 in (67 mm)
Rainy days1010111111151716148810
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)
Sunshine226 h232 h265 h278 h295 h250 h290 h322 h268 h264 h241 h235 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.