ClimateSearch

Tsuruoka, Yamagata

Japan · 125k people · 16 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 high37°F (3°C)38°F (3°C)44°F (7°C)55°F (13°C)66°F (19°C)72°F (22°C)79°F (26°C)81°F (27°C)75°F (24°C)65°F (18°C)54°F (12°C)43°F (6°C)
Average low31°F (-1°C)30°F (-1°C)34°F (1°C)42°F (5°C)52°F (11°C)60°F (16°C)69°F (20°C)71°F (22°C)65°F (18°C)54°F (12°C)44°F (7°C)35°F (2°C)
Dew point28°F (-2°C)28°F (-2°C)31°F (0°C)40°F (5°C)51°F (11°C)61°F (16°C)69°F (21°C)71°F (22°C)64°F (18°C)52°F (11°C)42°F (6°C)33°F (1°C)
Rainfall10.9 in (277 mm)7.3 in (185 mm)6.5 in (165 mm)5.1 in (129 mm)5.2 in (132 mm)5.8 in (148 mm)10.1 in (258 mm)7.9 in (201 mm)7.1 in (181 mm)8 in (203 mm)9.3 in (236 mm)11.8 in (300 mm)
Rainy days282321151413171616172126
Snowfall51.6 in (131.1 cm)34.3 in (87.2 cm)17.6 in (44.7 cm)2 in (5 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)3.4 in (8.7 cm)33.7 in (85.5 cm)
Sunshine191 h204 h262 h280 h295 h291 h272 h302 h248 h245 h191 h173 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

+2.6°F (+1.4°C)

Models range from +2.1°F (+1.2°C) to +3.2°F (+1.8°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.0°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.5°F (+1.4°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.7°F (+1.5°C)
  • September: +3.1°F (+1.7°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.1°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.