ClimateSearch

Jōetsu, Niigata

Japan · 189k people · 9 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 high40°F (4°C)41°F (5°C)47°F (8°C)59°F (15°C)70°F (21°C)76°F (24°C)82°F (28°C)85°F (29°C)77°F (25°C)67°F (20°C)57°F (14°C)46°F (8°C)
Average low30°F (-1°C)30°F (-1°C)33°F (1°C)42°F (6°C)53°F (12°C)62°F (16°C)70°F (21°C)72°F (22°C)65°F (19°C)55°F (13°C)44°F (7°C)35°F (1°C)
Dew point30°F (-1°C)30°F (-1°C)34°F (1°C)43°F (6°C)54°F (12°C)63°F (17°C)71°F (22°C)73°F (23°C)65°F (19°C)55°F (13°C)44°F (7°C)35°F (2°C)
Rainfall9.8 in (248 mm)7.3 in (185 mm)6.4 in (164 mm)4.5 in (115 mm)5 in (126 mm)6.4 in (162 mm)9.5 in (242 mm)7.7 in (194 mm)8.1 in (206 mm)7.5 in (190 mm)7.2 in (183 mm)9.6 in (244 mm)
Rainy days262120151416211917161823
Snowfall49 in (124.4 cm)36.3 in (92.3 cm)20.2 in (51.3 cm)3 in (7.7 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)3.8 in (9.6 cm)32.1 in (81.5 cm)
Sunshine220 h215 h268 h280 h306 h281 h286 h316 h247 h241 h205 h205 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 +2.0°F (+1.1°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.5°F (+1.4°C)
  • May: +1.9°F (+1.0°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.6°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.