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 high44°F (7°C)45°F (7°C)53°F (12°C)64°F (18°C)73°F (23°C)78°F (26°C)86°F (30°C)89°F (32°C)81°F (27°C)71°F (22°C)61°F (16°C)50°F (10°C)
Average low33°F (1°C)33°F (1°C)38°F (3°C)46°F (8°C)56°F (13°C)65°F (18°C)73°F (23°C)74°F (23°C)66°F (19°C)55°F (13°C)45°F (7°C)37°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)
Rainfall11 in (280 mm)6.6 in (168 mm)6.1 in (156 mm)5.4 in (137 mm)5.3 in (135 mm)6.5 in (165 mm)7.8 in (198 mm)4.7 in (120 mm)8 in (203 mm)6.6 in (168 mm)7.2 in (183 mm)11.8 in (301 mm)
Rainy days23181512111111711121522
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)
Sunshine138 h132 h165 h172 h180 h137 h155 h205 h154 h164 h142 h129 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.