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 high47°F (8°C)49°F (10°C)56°F (13°C)65°F (18°C)73°F (23°C)79°F (26°C)85°F (29°C)87°F (31°C)81°F (27°C)71°F (22°C)61°F (16°C)51°F (11°C)
Average low32°F (0°C)32°F (0°C)37°F (3°C)46°F (8°C)56°F (13°C)64°F (18°C)72°F (22°C)74°F (23°C)68°F (20°C)57°F (14°C)45°F (7°C)36°F (2°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)
Rainfall2.4 in (61 mm)3 in (76 mm)5.3 in (134 mm)5.8 in (148 mm)6.7 in (170 mm)9.5 in (242 mm)10.4 in (265 mm)6.7 in (170 mm)9.3 in (237 mm)8 in (204 mm)4.2 in (106 mm)2.6 in (65 mm)
Rainy days67111112161817141287
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)
Sunshine260 h242 h278 h275 h294 h257 h295 h326 h263 h250 h232 h247 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.