ClimateSearch

Toyota, Aichi

Japan · 426k people · 50 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)58°F (14°C)67°F (20°C)76°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 low33°F (1°C)34°F (1°C)40°F (4°C)49°F (9°C)58°F (14°C)66°F (19°C)73°F (23°C)75°F (24°C)69°F (21°C)58°F (14°C)47°F (8°C)37°F (3°C)
Dew point30°F (-1°C)30°F (-1°C)37°F (3°C)46°F (8°C)56°F (13°C)65°F (18°C)73°F (23°C)73°F (23°C)67°F (20°C)57°F (14°C)46°F (8°C)35°F (2°C)
Rainfall2.7 in (69 mm)3.3 in (83 mm)5.3 in (133 mm)6.8 in (173 mm)7.2 in (183 mm)8.8 in (223 mm)10 in (253 mm)7.1 in (180 mm)8.6 in (218 mm)7.9 in (202 mm)3.8 in (96 mm)2.7 in (68 mm)
Rainy days67101110121210101086
Snowfall0.7 in (1.9 cm)1.5 in (3.9 cm)0.2 in (0.4 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)
Sunshine192 h172 h190 h179 h173 h124 h156 h205 h161 h166 h167 h185 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 +1.7°F (+1.0°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

14 → 41

About 3.0× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.6°F (+1.4°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.6°F (+1.4°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.