ClimateSearch

Kani, Gifu

Japan · 102k people · 109 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 high47°F (8°C)49°F (9°C)56°F (13°C)66°F (19°C)74°F (23°C)79°F (26°C)86°F (30°C)89°F (32°C)82°F (28°C)72°F (22°C)62°F (16°C)51°F (11°C)
Average low32°F (0°C)33°F (0°C)38°F (3°C)47°F (8°C)56°F (14°C)64°F (18°C)72°F (22°C)74°F (23°C)67°F (20°C)56°F (13°C)45°F (7°C)36°F (2°C)
Dew point27°F (-3°C)28°F (-2°C)34°F (1°C)44°F (7°C)54°F (12°C)63°F (17°C)71°F (21°C)71°F (22°C)65°F (18°C)54°F (12°C)43°F (6°C)33°F (1°C)
Rainfall3.2 in (80 mm)3.4 in (87 mm)5.6 in (142 mm)7.2 in (184 mm)7.2 in (184 mm)8.9 in (227 mm)10.8 in (275 mm)7.4 in (189 mm)9.2 in (233 mm)7.4 in (187 mm)4 in (101 mm)3.2 in (81 mm)
Rainy days7710111112129101077
Snowfall1.4 in (3.6 cm)2 in (5.2 cm)0.2 in (0.6 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)0.7 in (1.7 cm)
Sunshine176 h164 h185 h175 h174 h125 h147 h197 h156 h167 h161 h168 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 +1.6°F (+0.9°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

10 → 30

About 2.9× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.1°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.6°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.3°F (+1.3°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.