ClimateSearch

Yokosuka, Kanagawa

Japan · 409k people · 13 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 (9°C)49°F (10°C)54°F (12°C)61°F (16°C)68°F (20°C)73°F (23°C)78°F (26°C)81°F (27°C)77°F (25°C)69°F (21°C)61°F (16°C)53°F (12°C)
Average low40°F (4°C)40°F (4°C)44°F (7°C)52°F (11°C)60°F (16°C)67°F (19°C)73°F (23°C)76°F (24°C)71°F (22°C)62°F (17°C)53°F (12°C)45°F (7°C)
Dew point31°F (0°C)32°F (0°C)38°F (4°C)48°F (9°C)57°F (14°C)65°F (18°C)72°F (22°C)74°F (23°C)67°F (20°C)57°F (14°C)47°F (9°C)37°F (3°C)
Rainfall2.9 in (74 mm)2.8 in (72 mm)5.2 in (131 mm)4.6 in (117 mm)5.2 in (131 mm)6.8 in (173 mm)5.9 in (149 mm)4.1 in (103 mm)7.4 in (187 mm)8.4 in (214 mm)3.9 in (98 mm)2.6 in (66 mm)
Rainy days781212111312111413108
Snowfall1.7 in (4.4 cm)2.5 in (6.4 cm)0.7 in (1.9 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 (0.2 cm)0.2 in (0.4 cm)
Sunshine247 h226 h250 h265 h277 h233 h277 h312 h244 h222 h208 h224 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 (+1.3°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.4°F (+1.4°C)
  • December: +2.0°F (+1.1°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.