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 high45°F (7°C)47°F (9°C)55°F (13°C)64°F (18°C)72°F (22°C)78°F (25°C)84°F (29°C)87°F (30°C)80°F (27°C)70°F (21°C)60°F (15°C)49°F (10°C)
Average low29°F (-2°C)29°F (-1°C)35°F (2°C)44°F (7°C)53°F (12°C)63°F (17°C)70°F (21°C)72°F (22°C)66°F (19°C)54°F (12°C)42°F (6°C)33°F (1°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)
Rainfall2.5 in (64 mm)2.9 in (73 mm)5.3 in (135 mm)6 in (152 mm)7 in (177 mm)8.6 in (220 mm)10.7 in (271 mm)6.2 in (157 mm)8.4 in (213 mm)7.2 in (182 mm)4 in (103 mm)2.7 in (68 mm)
Rainy days88111212151714131188
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)
Sunshine253 h237 h274 h269 h291 h254 h277 h313 h253 h249 h228 h239 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.