ClimateSearch

Takamatsu, Kagawa

Japan · 419k people · 9 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)55°F (13°C)63°F (17°C)71°F (22°C)76°F (25°C)83°F (28°C)85°F (30°C)79°F (26°C)70°F (21°C)61°F (16°C)51°F (11°C)
Average low38°F (3°C)38°F (3°C)42°F (6°C)51°F (10°C)59°F (15°C)67°F (19°C)74°F (24°C)76°F (25°C)71°F (21°C)61°F (16°C)51°F (10°C)42°F (6°C)
Dew point32°F (0°C)33°F (1°C)38°F (4°C)47°F (8°C)56°F (14°C)65°F (18°C)73°F (23°C)73°F (23°C)67°F (19°C)56°F (13°C)46°F (8°C)37°F (3°C)
Rainfall2.5 in (62 mm)2.6 in (67 mm)4.1 in (104 mm)4.4 in (111 mm)5.3 in (133 mm)7.8 in (199 mm)7.3 in (184 mm)4.7 in (119 mm)7.1 in (181 mm)5.7 in (145 mm)2.8 in (71 mm)2.7 in (67 mm)
Rainy days10101211101414111310910
Snowfall1.5 in (3.7 cm)1.9 in (4.7 cm)0.3 in (0.8 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 (1.4 cm)
Sunshine250 h240 h272 h277 h304 h256 h306 h330 h265 h257 h238 h250 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

+2.3°F (+1.3°C)

Models range from +1.6°F (+0.9°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.0°F (+1.1°C)
  • February: +1.9°F (+1.0°C)
  • March: +1.9°F (+1.0°C)
  • April: +2.4°F (+1.3°C)
  • May: +1.7°F (+0.9°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.4°F (+1.4°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.4°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.