ClimateSearch

Kotō, Kumamoto

Japan · 544k people · 12 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 high48°F (9°C)51°F (11°C)57°F (14°C)66°F (19°C)74°F (23°C)78°F (26°C)84°F (29°C)87°F (31°C)82°F (28°C)73°F (23°C)62°F (17°C)52°F (11°C)
Average low37°F (3°C)38°F (3°C)43°F (6°C)51°F (10°C)59°F (15°C)67°F (19°C)74°F (23°C)75°F (24°C)69°F (21°C)59°F (15°C)49°F (10°C)40°F (5°C)
Dew point34°F (1°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (14°C)66°F (19°C)73°F (23°C)73°F (23°C)67°F (20°C)57°F (14°C)48°F (9°C)38°F (3°C)
Rainfall3 in (77 mm)3.9 in (100 mm)5.6 in (141 mm)6.1 in (156 mm)7 in (178 mm)16.1 in (408 mm)12.3 in (312 mm)5.5 in (141 mm)6.4 in (164 mm)3.9 in (99 mm)3.7 in (94 mm)3.3 in (83 mm)
Rainy days1110131212171713129910
Snowfall1.3 in (3.2 cm)0.8 in (2.1 cm)0.2 in (0.4 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)0.6 in (1.5 cm)
Sunshine211 h217 h239 h255 h269 h205 h271 h306 h255 h257 h226 h221 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

+1.9°F (+1.1°C)

Models range from +1.6°F (+0.9°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

11 26

About 2.3× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.4°F (+1.4°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.7°F (+0.9°C)
  • July: +2.1°F (+1.2°C)
  • August: +1.9°F (+1.1°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.5°F (+1.4°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.