ClimateSearch

Aizu-Wakamatsu, Fukushima

Japan · 118k people · 238 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 high38°F (3°C)40°F (4°C)48°F (9°C)62°F (17°C)72°F (22°C)77°F (25°C)83°F (29°C)86°F (30°C)78°F (26°C)67°F (19°C)55°F (13°C)44°F (7°C)
Average low26°F (-3°C)26°F (-3°C)31°F (0°C)41°F (5°C)51°F (11°C)60°F (16°C)68°F (20°C)69°F (21°C)62°F (17°C)50°F (10°C)39°F (4°C)31°F (0°C)
Dew point27°F (-3°C)26°F (-3°C)31°F (-1°C)40°F (4°C)51°F (10°C)60°F (16°C)68°F (20°C)70°F (21°C)63°F (17°C)52°F (11°C)42°F (5°C)32°F (0°C)
Rainfall4.1 in (104 mm)2.7 in (69 mm)3.1 in (79 mm)3.2 in (82 mm)3.1 in (79 mm)4.5 in (114 mm)6.6 in (167 mm)4.8 in (121 mm)5.3 in (134 mm)5.1 in (128 mm)3.2 in (80 mm)4.2 in (106 mm)
Rainy days1713131110101189101217
Snowfall25.4 in (64.4 cm)17.9 in (45.5 cm)14.2 in (36.1 cm)3.3 in (8.3 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)2.2 in (5.7 cm)16.2 in (41.2 cm)
Sunshine112 h116 h145 h153 h150 h113 h105 h140 h107 h114 h102 h101 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

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +1.8°F (+1.0°C)
  • March: +2.0°F (+1.1°C)
  • April: +3.0°F (+1.7°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.8°F (+1.0°C)
  • August: +2.5°F (+1.4°C)
  • September: +3.2°F (+1.8°C)
  • October: +2.6°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.