ClimateSearch

Hirosaki, Aomori

Japan · 169k people · 44 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 high34°F (1°C)36°F (2°C)43°F (6°C)57°F (14°C)67°F (19°C)73°F (23°C)79°F (26°C)83°F (28°C)76°F (25°C)65°F (18°C)53°F (11°C)39°F (4°C)
Average low24°F (-5°C)25°F (-4°C)31°F (-1°C)40°F (4°C)50°F (10°C)58°F (15°C)67°F (19°C)69°F (21°C)61°F (16°C)49°F (9°C)38°F (3°C)28°F (-2°C)
Dew point21°F (-6°C)22°F (-6°C)27°F (-3°C)37°F (3°C)49°F (9°C)58°F (15°C)67°F (19°C)68°F (20°C)60°F (16°C)48°F (9°C)36°F (2°C)26°F (-4°C)
Rainfall4.7 in (119 mm)3.9 in (98 mm)3.6 in (92 mm)3.3 in (84 mm)3.4 in (86 mm)3.9 in (98 mm)5.8 in (148 mm)5.6 in (143 mm)5.9 in (150 mm)5.2 in (132 mm)4.8 in (123 mm)5.2 in (132 mm)
Rainy days171515121110101010131517
Snowfall22.8 in (58 cm)20.6 in (52.2 cm)17.4 in (44.1 cm)3.7 in (9.5 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.1 in (0.2 cm)5.5 in (13.9 cm)20.2 in (51.4 cm)
Sunshine113 h119 h161 h171 h166 h152 h124 h148 h133 h149 h113 h104 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 +1.9°F (+1.1°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.2°F (+1.2°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.8°F (+1.6°C)
  • September: +3.3°F (+1.8°C)
  • October: +2.6°F (+1.4°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.