ClimateSearch

Inazawa, Aichi

Japan · 135k people · 6 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 high46°F (8°C)48°F (9°C)55°F (13°C)64°F (18°C)73°F (23°C)78°F (26°C)84°F (29°C)87°F (31°C)80°F (27°C)70°F (21°C)60°F (16°C)50°F (10°C)
Average low30°F (-1°C)30°F (-1°C)36°F (2°C)45°F (7°C)54°F (12°C)64°F (18°C)71°F (22°C)73°F (23°C)67°F (19°C)55°F (13°C)44°F (7°C)35°F (1°C)
Dew point29°F (-2°C)29°F (-2°C)35°F (2°C)44°F (7°C)55°F (13°C)64°F (18°C)71°F (22°C)72°F (22°C)66°F (19°C)55°F (13°C)44°F (7°C)34°F (1°C)
Rainfall2.5 in (63 mm)2.8 in (70 mm)4.9 in (125 mm)5.8 in (146 mm)6.8 in (174 mm)8.8 in (224 mm)10.8 in (275 mm)7 in (177 mm)9.8 in (248 mm)7.8 in (197 mm)3.9 in (99 mm)2.6 in (65 mm)
Rainy days77111112151815141287
Snowfall0.9 in (2.2 cm)1.6 in (4.1 cm)0.1 in (0.2 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)0.4 in (1 cm)
Sunshine257 h241 h277 h270 h294 h256 h287 h321 h257 h250 h231 h245 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 +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

12 35

About 3.0× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°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: +2.1°F (+1.2°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.6°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.5°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.