ClimateSearch

Iida, Nagano

Japan · 102k people · 515 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)42°F (6°C)50°F (10°C)62°F (16°C)70°F (21°C)76°F (24°C)82°F (28°C)84°F (29°C)78°F (25°C)68°F (20°C)57°F (14°C)46°F (8°C)
Average low24°F (-5°C)25°F (-4°C)33°F (0°C)42°F (6°C)52°F (11°C)61°F (16°C)68°F (20°C)70°F (21°C)63°F (17°C)52°F (11°C)41°F (5°C)31°F (-1°C)
Dew point23°F (-5°C)24°F (-4°C)32°F (0°C)42°F (6°C)52°F (11°C)62°F (16°C)69°F (21°C)70°F (21°C)64°F (18°C)53°F (12°C)41°F (5°C)30°F (-1°C)
Rainfall3.9 in (98 mm)4.3 in (109 mm)6.8 in (173 mm)7 in (179 mm)7.9 in (199 mm)10.5 in (268 mm)12.2 in (311 mm)7.3 in (185 mm)9.2 in (234 mm)8.6 in (218 mm)5 in (127 mm)4 in (101 mm)
Rainy days121013131418201916131012
Snowfall14.6 in (37.1 cm)12.5 in (31.7 cm)9.4 in (23.8 cm)1.6 in (4 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0.1 cm)1 in (2.5 cm)9.1 in (23.1 cm)
Sunshine257 h238 h273 h272 h287 h248 h273 h309 h250 h247 h227 h240 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

+2.1°F (+1.2°C)

Models range from +1.6°F (+0.9°C) to +2.5°F (+1.4°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: +2.0°F (+1.1°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.0°F (+1.1°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.