ClimateSearch

Fujinomiya, Shizuoka

Japan · 133k people · 114 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 high48°F (9°C)49°F (9°C)55°F (13°C)63°F (17°C)70°F (21°C)75°F (24°C)81°F (27°C)83°F (28°C)78°F (26°C)70°F (21°C)61°F (16°C)52°F (11°C)
Average low34°F (1°C)34°F (1°C)39°F (4°C)47°F (9°C)56°F (13°C)64°F (18°C)71°F (22°C)73°F (23°C)67°F (20°C)58°F (15°C)48°F (9°C)39°F (4°C)
Dew point30°F (-1°C)31°F (0°C)38°F (3°C)47°F (9°C)56°F (14°C)64°F (18°C)72°F (22°C)73°F (23°C)67°F (20°C)57°F (14°C)47°F (8°C)36°F (2°C)
Rainfall3.9 in (100 mm)4.8 in (121 mm)8.7 in (221 mm)9.1 in (231 mm)9.2 in (233 mm)12.4 in (315 mm)14.4 in (365 mm)9.8 in (250 mm)13.4 in (341 mm)11.2 in (285 mm)6.5 in (165 mm)4.2 in (106 mm)
Rainy days101116161621242319161210
Snowfall8.2 in (20.8 cm)9.5 in (24.1 cm)7 in (17.9 cm)0.9 in (2.2 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)2.3 in (5.9 cm)
Sunshine259 h238 h271 h270 h283 h242 h280 h313 h251 h241 h224 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

2 3

About 1.8× 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: +2.0°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°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.