ClimateSearch

Kasuga, Fukuoka

Japan · 111k people · 43 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 (9°C)50°F (10°C)57°F (14°C)66°F (19°C)75°F (24°C)80°F (27°C)85°F (30°C)88°F (31°C)81°F (27°C)72°F (22°C)62°F (17°C)52°F (11°C)
Average low36°F (2°C)36°F (2°C)41°F (5°C)49°F (9°C)58°F (14°C)66°F (19°C)74°F (23°C)75°F (24°C)68°F (20°C)58°F (14°C)48°F (9°C)39°F (4°C)
Dew point33°F (1°C)35°F (1°C)40°F (5°C)49°F (9°C)58°F (14°C)67°F (19°C)74°F (23°C)74°F (24°C)68°F (20°C)57°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.5 in (63 mm)2.9 in (74 mm)4.6 in (117 mm)5.2 in (131 mm)5.8 in (147 mm)12 in (304 mm)11.4 in (289 mm)6.7 in (170 mm)7.4 in (188 mm)4 in (100 mm)3.4 in (86 mm)2.8 in (70 mm)
Rainy days1010121111161815138910
Snowfall1.3 in (3.2 cm)0.9 in (2.4 cm)0.2 in (0.5 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)0.5 in (1.3 cm)
Sunshine197 h214 h245 h263 h279 h225 h272 h308 h259 h259 h228 h209 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

+2.2°F (+1.2°C)

Models range from +2.0°F (+1.1°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

17 47

About 2.8× as many

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.7°F (+0.9°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.1°F (+1.2°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.