ClimateSearch

Tajimi, Gifu

Japan · 108k people · 131 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)50°F (10°C)
Average low29°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 (22°C)73°F (23°C)66°F (19°C)55°F (13°C)43°F (6°C)33°F (1°C)
Dew point28°F (-2°C)28°F (-2°C)34°F (1°C)44°F (7°C)54°F (12°C)63°F (17°C)71°F (22°C)71°F (22°C)65°F (19°C)55°F (13°C)43°F (6°C)33°F (1°C)
Rainfall2.6 in (66 mm)3.1 in (79 mm)5.4 in (137 mm)5.9 in (150 mm)7 in (177 mm)9.2 in (233 mm)10.5 in (266 mm)6.6 in (168 mm)9 in (229 mm)8 in (203 mm)4.1 in (105 mm)2.8 in (70 mm)
Rainy days88111213171916151298
Snowfall2.2 in (5.7 cm)2.8 in (7 cm)0.6 in (1.6 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)0 in (0 cm)0 in (0 cm)0.9 in (2.2 cm)
Sunshine258 h241 h277 h273 h293 h256 h286 h321 h260 h251 h231 h245 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

+2.3°F (+1.3°C)

Models range from +1.7°F (+1.0°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

10 22

About 2.2× as many

Warming by month
  • January: +2.4°F (+1.4°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.4°F (+1.4°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: +2.2°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.