ClimateSearch

Fukui-shi, Fukui

Japan · 262k people · 18 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 high42°F (6°C)43°F (6°C)50°F (10°C)60°F (15°C)68°F (20°C)74°F (24°C)81°F (27°C)84°F (29°C)77°F (25°C)68°F (20°C)58°F (15°C)48°F (9°C)
Average low33°F (0°C)32°F (0°C)37°F (3°C)46°F (8°C)55°F (13°C)63°F (17°C)72°F (22°C)74°F (23°C)67°F (20°C)57°F (14°C)47°F (8°C)38°F (3°C)
Dew point30°F (-1°C)30°F (-1°C)35°F (2°C)44°F (7°C)54°F (12°C)63°F (17°C)71°F (21°C)72°F (22°C)65°F (18°C)54°F (12°C)44°F (7°C)35°F (2°C)
Rainfall8.2 in (208 mm)5.9 in (150 mm)6.5 in (165 mm)5.8 in (148 mm)6.4 in (164 mm)7.7 in (196 mm)10.6 in (270 mm)6.7 in (171 mm)8.9 in (225 mm)6.7 in (171 mm)6.8 in (172 mm)8.6 in (219 mm)
Rainy days231817141314171314131622
Snowfall24.8 in (63 cm)18 in (45.7 cm)7.1 in (18 cm)0.6 in (1.5 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)0.6 in (1.4 cm)14 in (35.6 cm)
Sunshine237 h226 h270 h274 h301 h269 h292 h323 h258 h254 h223 h221 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

+2.1°F (+1.2°C)

Models range from +1.7°F (+1.0°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.9°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.6°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.