ClimateSearch

Kakegawa, Shizuoka

Japan · 118k people · 30 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 (12°C)59°F (15°C)67°F (19°C)73°F (23°C)78°F (26°C)85°F (29°C)87°F (31°C)82°F (28°C)73°F (23°C)65°F (18°C)55°F (13°C)
Average low35°F (2°C)36°F (2°C)42°F (6°C)51°F (11°C)59°F (15°C)67°F (19°C)74°F (23°C)75°F (24°C)70°F (21°C)60°F (16°C)49°F (10°C)39°F (4°C)
Dew point30°F (-1°C)31°F (-1°C)37°F (3°C)46°F (8°C)56°F (13°C)65°F (18°C)72°F (22°C)73°F (23°C)68°F (20°C)58°F (14°C)47°F (9°C)36°F (2°C)
Rainfall3.3 in (85 mm)4.2 in (106 mm)6.5 in (165 mm)7.4 in (188 mm)8 in (202 mm)10.9 in (278 mm)9.9 in (252 mm)6.7 in (169 mm)9.3 in (236 mm)9.9 in (252 mm)5.5 in (139 mm)3.6 in (92 mm)
Rainy days6711111012119111197
Snowfall0.1 in (0.3 cm)0.3 in (0.8 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)
Sunshine200 h174 h186 h177 h167 h119 h158 h204 h161 h158 h163 h190 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 +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

7 → 13

About 2.0× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.6°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.8°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: +2.7°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.