ClimateSearch

Toyohashi, Aichi

Japan · 377k people · 10 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 high48°F (9°C)50°F (10°C)56°F (13°C)65°F (18°C)72°F (22°C)77°F (25°C)84°F (29°C)86°F (30°C)81°F (27°C)71°F (22°C)62°F (17°C)52°F (11°C)
Average low34°F (1°C)35°F (1°C)39°F (4°C)48°F (9°C)57°F (14°C)65°F (18°C)73°F (23°C)75°F (24°C)69°F (20°C)58°F (15°C)48°F (9°C)38°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)3.2 in (82 mm)5.4 in (138 mm)6 in (153 mm)6.8 in (174 mm)9.8 in (250 mm)9.7 in (247 mm)5.6 in (142 mm)9.4 in (239 mm)8.3 in (210 mm)4.5 in (114 mm)2.7 in (68 mm)
Rainy days67111011161615141296
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)
Sunshine259 h240 h273 h271 h289 h250 h296 h322 h261 h244 h228 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

+2.2°F (+1.2°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 21

About 2.2× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.3°F (+1.3°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.6°F (+1.4°C)
  • December: +2.1°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.