ClimateSearch

Toyokawa, Aichi

Japan · 185k people · 8 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 (10°C)51°F (11°C)58°F (14°C)67°F (19°C)74°F (24°C)79°F (26°C)86°F (30°C)89°F (32°C)83°F (28°C)74°F (23°C)64°F (18°C)54°F (12°C)
Average low35°F (2°C)36°F (2°C)41°F (5°C)50°F (10°C)58°F (15°C)67°F (19°C)74°F (23°C)76°F (24°C)70°F (21°C)59°F (15°C)48°F (9°C)39°F (4°C)
Dew point30°F (-1°C)31°F (-1°C)37°F (3°C)46°F (8°C)56°F (13°C)65°F (18°C)72°F (22°C)73°F (23°C)67°F (20°C)57°F (14°C)46°F (8°C)36°F (2°C)
Rainfall2.5 in (64 mm)3.3 in (83 mm)5.2 in (131 mm)6.6 in (168 mm)7.3 in (186 mm)9.1 in (232 mm)9.2 in (233 mm)6.6 in (168 mm)7.8 in (199 mm)8.7 in (220 mm)4.3 in (108 mm)2.7 in (69 mm)
Rainy days5610101012119101086
Snowfall0.2 in (0.4 cm)0.5 in (1.2 cm)0 in (0.1 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 in (0 cm)
Sunshine196 h173 h189 h179 h170 h121 h159 h207 h162 h162 h166 h187 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 +1.8°F (+1.0°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

10 → 25

About 2.7× as many

Warming by month
  • January: +2.4°F (+1.4°C)
  • February: +2.1°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.4°F (+1.3°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.6°F (+1.5°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.