ClimateSearch

Fuji, Shizuoka

Japan · 245k people · 8 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)50°F (10°C)56°F (13°C)64°F (18°C)71°F (22°C)76°F (25°C)83°F (28°C)85°F (29°C)80°F (27°C)71°F (22°C)63°F (17°C)54°F (12°C)
Average low36°F (2°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (14°C)65°F (19°C)73°F (23°C)74°F (24°C)69°F (21°C)60°F (16°C)50°F (10°C)41°F (5°C)
Dew point32°F (0°C)33°F (1°C)40°F (5°C)49°F (10°C)58°F (15°C)66°F (19°C)73°F (23°C)75°F (24°C)69°F (21°C)59°F (15°C)49°F (9°C)38°F (3°C)
Rainfall3.9 in (100 mm)4.6 in (116 mm)8 in (204 mm)8 in (202 mm)7.8 in (199 mm)10.6 in (270 mm)11.9 in (302 mm)7.9 in (201 mm)11.4 in (290 mm)10.1 in (257 mm)5.7 in (146 mm)3.9 in (100 mm)
Rainy days111216141518201916151210
Snowfall7.2 in (18.4 cm)8.3 in (21 cm)5 in (12.7 cm)0.5 in (1.3 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)1.5 in (3.7 cm)
Sunshine259 h238 h270 h271 h285 h242 h283 h316 h253 h241 h223 h241 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

4 7

About 1.9× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.3°F (+1.3°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.6°F (+1.4°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.7°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.