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 high65°F (18°C)65°F (18°C)68°F (20°C)71°F (22°C)76°F (24°C)80°F (27°C)84°F (29°C)84°F (29°C)82°F (28°C)78°F (26°C)73°F (23°C)68°F (20°C)
Average low60°F (16°C)60°F (16°C)62°F (17°C)67°F (19°C)71°F (22°C)77°F (25°C)80°F (27°C)80°F (27°C)78°F (26°C)74°F (24°C)70°F (21°C)64°F (18°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)
Rainfall3.9 in (99 mm)3.8 in (97 mm)5.1 in (128 mm)5.9 in (149 mm)8.5 in (216 mm)8.6 in (218 mm)5.1 in (129 mm)6.9 in (175 mm)7.9 in (199 mm)5.5 in (139 mm)3.9 in (100 mm)4.1 in (105 mm)
Rainy days121113131416131615121111
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)
Sunshine180 h183 h236 h266 h284 h289 h361 h350 h303 h285 h228 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

+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.