ClimateSearch

Ginowan, Okinawa

Japan · 100k people · 106 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 high67°F (19°C)67°F (19°C)70°F (21°C)74°F (24°C)79°F (26°C)84°F (29°C)88°F (31°C)88°F (31°C)86°F (30°C)82°F (28°C)76°F (24°C)70°F (21°C)
Average low57°F (14°C)58°F (14°C)60°F (16°C)65°F (18°C)71°F (21°C)76°F (24°C)79°F (26°C)79°F (26°C)77°F (25°C)73°F (23°C)67°F (20°C)61°F (16°C)
Dew point51°F (10°C)52°F (11°C)55°F (13°C)61°F (16°C)67°F (20°C)74°F (24°C)76°F (25°C)76°F (24°C)73°F (23°C)67°F (20°C)61°F (16°C)54°F (12°C)
Rainfall4.2 in (107 mm)4 in (102 mm)5.9 in (150 mm)7.4 in (188 mm)10 in (255 mm)10.5 in (268 mm)7 in (177 mm)9.8 in (248 mm)10.6 in (269 mm)7.7 in (196 mm)4.4 in (113 mm)4.6 in (118 mm)
Rainy days11101111111171010889
Snowfall0 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 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine95 h98 h135 h154 h156 h150 h231 h231 h201 h191 h142 h107 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

+1.7°F (+0.9°C)

Models range from +1.6°F (+0.9°C) to +1.7°F (+1.0°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +1.6°F (+0.9°C)
  • February: +1.7°F (+1.0°C)
  • March: +1.6°F (+0.9°C)
  • April: +1.4°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.7°F (+1.0°C)
  • September: +1.9°F (+1.0°C)
  • October: +1.9°F (+1.1°C)
  • November: +1.6°F (+0.9°C)
  • December: +1.7°F (+1.0°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.