ClimateSearch

Tsuyama, Okayama

Japan · 102k people · 99 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 high45°F (7°C)47°F (8°C)55°F (13°C)65°F (18°C)73°F (23°C)79°F (26°C)85°F (30°C)87°F (31°C)80°F (27°C)70°F (21°C)60°F (16°C)50°F (10°C)
Average low31°F (-1°C)31°F (0°C)36°F (2°C)45°F (7°C)55°F (13°C)63°F (17°C)72°F (22°C)73°F (23°C)66°F (19°C)54°F (12°C)44°F (6°C)35°F (2°C)
Dew point31°F (-1°C)31°F (0°C)37°F (3°C)45°F (7°C)55°F (13°C)64°F (18°C)73°F (23°C)73°F (23°C)66°F (19°C)55°F (13°C)45°F (7°C)36°F (2°C)
Rainfall1.8 in (47 mm)2.3 in (58 mm)4.3 in (110 mm)4.8 in (122 mm)5.6 in (144 mm)7.6 in (192 mm)9.3 in (236 mm)5.6 in (142 mm)7.2 in (182 mm)4.5 in (115 mm)2.5 in (63 mm)2.1 in (53 mm)
Rainy days6811111113161412867
Snowfall1.9 in (4.9 cm)2.5 in (6.4 cm)0.9 in (2.2 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)0.9 in (2.3 cm)
Sunshine241 h234 h272 h277 h307 h268 h303 h326 h268 h260 h239 h239 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

+2.1°F (+1.2°C)

Models range from +1.7°F (+1.0°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

15 37

About 2.4× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.9°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.6°F (+1.4°C)
  • December: +2.3°F (+1.3°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.