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 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 (1°C)38°F (3°C)47°F (9°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 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)
Rainfall3 in (75 mm)3.4 in (87 mm)5.6 in (141 mm)7.3 in (184 mm)7.3 in (185 mm)9 in (228 mm)10.7 in (273 mm)7.8 in (197 mm)9.3 in (237 mm)7.6 in (194 mm)3.9 in (98 mm)3 in (77 mm)
Rainy days77111111121310111087
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)
Sunshine184 h168 h188 h177 h172 h124 h150 h201 h158 h165 h164 h177 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.