ClimateSearch

Okazaki, Aichi

Japan · 385k people · 28 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 (11°C)58°F (14°C)67°F (20°C)75°F (24°C)81°F (27°C)87°F (31°C)90°F (32°C)83°F (29°C)74°F (23°C)64°F (18°C)54°F (12°C)
Average low34°F (1°C)35°F (2°C)40°F (5°C)49°F (10°C)58°F (15°C)67°F (19°C)74°F (23°C)76°F (24°C)69°F (21°C)58°F (15°C)47°F (9°C)38°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)
Rainfall2.6 in (65 mm)3.2 in (82 mm)5.1 in (130 mm)6.6 in (167 mm)7.1 in (181 mm)8.8 in (224 mm)9.5 in (241 mm)6.8 in (173 mm)8.3 in (211 mm)8.2 in (208 mm)3.9 in (98 mm)2.6 in (66 mm)
Rainy days67101010121210101086
Snowfall0.8 in (2 cm)1.5 in (3.8 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 (0.4 cm)
Sunshine193 h173 h190 h179 h173 h124 h156 h205 h161 h166 h167 h186 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 +3.0°F (+1.7°C)

Days above 90°F (32°C) a year

11 → 32

About 2.8× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.6°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.