ClimateSearch

Karatsu, Saga

Japan · 118k people · 5 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)50°F (10°C)56°F (14°C)65°F (18°C)73°F (23°C)78°F (26°C)84°F (29°C)87°F (30°C)80°F (27°C)72°F (22°C)62°F (17°C)53°F (11°C)
Average low40°F (4°C)40°F (5°C)44°F (7°C)52°F (11°C)60°F (15°C)67°F (20°C)75°F (24°C)77°F (25°C)71°F (22°C)62°F (17°C)52°F (11°C)44°F (7°C)
Dew point34°F (1°C)35°F (2°C)41°F (5°C)49°F (10°C)58°F (15°C)67°F (20°C)74°F (24°C)75°F (24°C)68°F (20°C)57°F (14°C)48°F (9°C)38°F (3°C)
Rainfall3 in (77 mm)3.1 in (80 mm)4.9 in (124 mm)5.4 in (136 mm)5.5 in (141 mm)11 in (279 mm)10.4 in (264 mm)6.5 in (165 mm)7.4 in (187 mm)4.1 in (104 mm)3.7 in (95 mm)3.2 in (81 mm)
Rainy days12111211101516141381011
Snowfall1 in (2.5 cm)0.7 in (1.7 cm)0.1 in (0.3 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)0.2 in (0.5 cm)
Sunshine190 h211 h246 h267 h282 h229 h276 h311 h261 h264 h228 h204 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

+2.0°F (+1.1°C)

Models range from +1.9°F (+1.0°C) to +2.1°F (+1.1°C)

Days above 90°F (32°C) a year

8 23

About 3.1× as many

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.6°F (+0.9°C)
  • June: +1.8°F (+1.0°C)
  • July: +2.1°F (+1.1°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.1°F (+1.2°C)
  • December: +2.2°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.