ClimateSearch

Shizuoka, Shizuoka

Japan · 693k people · 24 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 high52°F (11°C)54°F (12°C)59°F (15°C)67°F (19°C)74°F (23°C)78°F (26°C)85°F (29°C)87°F (31°C)82°F (28°C)74°F (23°C)65°F (19°C)56°F (14°C)
Average low35°F (2°C)37°F (3°C)42°F (6°C)51°F (10°C)58°F (15°C)66°F (19°C)73°F (23°C)74°F (24°C)69°F (21°C)60°F (15°C)49°F (10°C)39°F (4°C)
Dew point31°F (0°C)32°F (0°C)39°F (4°C)48°F (9°C)57°F (14°C)65°F (19°C)73°F (23°C)74°F (23°C)68°F (20°C)58°F (15°C)48°F (9°C)37°F (3°C)
Rainfall2.8 in (72 mm)3.8 in (97 mm)6.6 in (167 mm)7.6 in (194 mm)7.7 in (196 mm)10 in (253 mm)10.5 in (267 mm)7.8 in (199 mm)9.5 in (241 mm)7.8 in (197 mm)4.7 in (119 mm)2.9 in (74 mm)
Rainy days78131211121191010107
Snowfall0.4 in (1 cm)1 in (2.6 cm)0.3 in (0.8 cm)0 in (0.1 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)0.1 in (0.3 cm)
Sunshine195 h169 h180 h170 h163 h116 h153 h202 h157 h157 h158 h182 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

+2.2°F (+1.2°C)

Models range from +1.7°F (+0.9°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

3 → 6

About 2.0× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.0°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.5°F (+1.4°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.2°F (+1.2°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.