ClimateSearch

Hamamatsu, Shizuoka

Japan · 792k people · 5 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 high51°F (10°C)53°F (11°C)59°F (15°C)68°F (20°C)75°F (24°C)79°F (26°C)86°F (30°C)89°F (32°C)83°F (28°C)74°F (24°C)65°F (18°C)55°F (13°C)
Average low36°F (2°C)37°F (3°C)43°F (6°C)51°F (11°C)59°F (15°C)67°F (19°C)74°F (23°C)76°F (24°C)70°F (21°C)60°F (16°C)50°F (10°C)40°F (5°C)
Dew point30°F (-1°C)31°F (-1°C)37°F (3°C)47°F (8°C)56°F (14°C)65°F (18°C)72°F (22°C)73°F (23°C)68°F (20°C)57°F (14°C)47°F (8°C)36°F (2°C)
Rainfall2.6 in (67 mm)3.4 in (87 mm)5.5 in (139 mm)6.8 in (173 mm)7.8 in (197 mm)10.1 in (257 mm)9.5 in (242 mm)6.3 in (159 mm)7.5 in (190 mm)9.2 in (233 mm)4.9 in (124 mm)3.1 in (79 mm)
Rainy days5710101012119101196
Snowfall0.2 in (0.4 cm)0.4 in (1 cm)0.1 in (0.2 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 in (0 cm)0 in (0 cm)0 in (0.1 cm)
Sunshine198 h173 h186 h176 h166 h118 h157 h204 h160 h157 h164 h188 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 +1.8°F (+1.0°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

9 → 26

About 2.7× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.1°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: +2.2°F (+1.2°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.1°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.