ClimateSearch

Ōgaki, Gifu

Japan · 162k people · 8 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 high48°F (9°C)49°F (10°C)56°F (14°C)66°F (19°C)75°F (24°C)81°F (27°C)87°F (31°C)90°F (32°C)83°F (28°C)73°F (23°C)63°F (17°C)52°F (11°C)
Average low34°F (1°C)34°F (1°C)39°F (4°C)48°F (9°C)57°F (14°C)66°F (19°C)74°F (23°C)75°F (24°C)68°F (20°C)57°F (14°C)46°F (8°C)37°F (3°C)
Dew point30°F (-1°C)30°F (-1°C)36°F (2°C)45°F (7°C)55°F (13°C)64°F (18°C)72°F (22°C)73°F (23°C)67°F (19°C)56°F (13°C)45°F (7°C)35°F (2°C)
Rainfall3.5 in (89 mm)3.5 in (89 mm)5.1 in (129 mm)6.4 in (163 mm)6.7 in (171 mm)8.6 in (218 mm)9.4 in (240 mm)5.4 in (138 mm)8 in (204 mm)6.3 in (159 mm)3.7 in (95 mm)3.5 in (88 mm)
Rainy days991111101212810978
Snowfall2.7 in (6.8 cm)3.3 in (8.3 cm)0.7 in (1.7 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)1.5 in (3.7 cm)
Sunshine172 h161 h181 h172 h172 h125 h150 h199 h155 h166 h161 h167 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 +1.8°F (+1.0°C) to +2.6°F (+1.5°C)

Days above 90°F (32°C) a year

11 → 30

About 2.8× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.1°F (+1.2°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.1°F (+1.1°C)
  • June: +2.1°F (+1.1°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.7°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.