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 high47°F (8°C)49°F (9°C)56°F (14°C)66°F (19°C)75°F (24°C)81°F (27°C)87°F (31°C)90°F (32°C)82°F (28°C)72°F (22°C)62°F (16°C)51°F (11°C)
Average low31°F (0°C)32°F (0°C)36°F (2°C)45°F (7°C)55°F (13°C)64°F (18°C)73°F (23°C)74°F (23°C)66°F (19°C)55°F (13°C)44°F (7°C)36°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)
Rainfall2.2 in (57 mm)2.4 in (60 mm)4 in (103 mm)4.8 in (122 mm)5.6 in (143 mm)7 in (178 mm)8.8 in (224 mm)4.4 in (111 mm)8.1 in (206 mm)4.8 in (122 mm)2.8 in (71 mm)2.4 in (61 mm)
Rainy days6710109101169766
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)
Sunshine155 h148 h172 h176 h187 h134 h163 h205 h165 h175 h162 h159 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.