ClimateSearch

Niigata, Niigata

Japan · 798k people · 4 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)40°F (5°C)47°F (9°C)57°F (14°C)67°F (19°C)74°F (23°C)80°F (27°C)83°F (28°C)77°F (25°C)66°F (19°C)56°F (13°C)46°F (8°C)
Average low32°F (0°C)31°F (0°C)35°F (2°C)43°F (6°C)53°F (11°C)62°F (17°C)70°F (21°C)73°F (23°C)67°F (19°C)56°F (13°C)46°F (8°C)37°F (3°C)
Dew point29°F (-2°C)28°F (-2°C)32°F (0°C)41°F (5°C)52°F (11°C)62°F (16°C)70°F (21°C)71°F (22°C)64°F (18°C)53°F (12°C)42°F (6°C)34°F (1°C)
Rainfall7 in (178 mm)4.7 in (120 mm)4.7 in (120 mm)3.6 in (93 mm)3.8 in (96 mm)4.7 in (120 mm)8.5 in (215 mm)5.9 in (150 mm)5.6 in (142 mm)5.8 in (147 mm)6.2 in (158 mm)7.4 in (189 mm)
Rainy days252019141212161414151924
Snowfall22.8 in (57.9 cm)15.8 in (40.2 cm)5.7 in (14.6 cm)0.6 in (1.4 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)0.5 in (1.3 cm)11.3 in (28.7 cm)
Sunshine196 h208 h262 h280 h302 h292 h287 h320 h255 h246 h199 h184 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 +3.1°F (+1.7°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.0°F (+1.1°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.6°F (+1.5°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.6°F (+1.5°C)
  • September: +3.0°F (+1.7°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.5°F (+1.4°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.