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 high49°F (9°C)51°F (10°C)57°F (14°C)67°F (19°C)75°F (24°C)81°F (27°C)87°F (31°C)90°F (32°C)83°F (29°C)73°F (23°C)63°F (17°C)53°F (12°C)
Average low35°F (2°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (15°C)67°F (19°C)75°F (24°C)76°F (25°C)69°F (21°C)58°F (15°C)48°F (9°C)38°F (3°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)
Rainfall1.6 in (40 mm)1.9 in (49 mm)3.6 in (92 mm)5 in (127 mm)5.7 in (146 mm)8.4 in (213 mm)8.5 in (217 mm)4.8 in (122 mm)9.4 in (240 mm)6 in (153 mm)2.7 in (68 mm)1.6 in (42 mm)
Rainy days78101091110610876
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)
Sunshine167 h158 h177 h178 h187 h128 h176 h217 h167 h176 h165 h171 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.