ClimateSearch

Nasushiobara, Tochigi

Japan · 116k people · 289 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 (5°C)42°F (5°C)49°F (9°C)60°F (15°C)69°F (20°C)74°F (23°C)80°F (27°C)82°F (28°C)75°F (24°C)65°F (18°C)55°F (13°C)45°F (7°C)
Average low26°F (-3°C)27°F (-3°C)32°F (0°C)41°F (5°C)51°F (10°C)59°F (15°C)67°F (19°C)69°F (21°C)62°F (17°C)51°F (11°C)40°F (5°C)31°F (0°C)
Dew point24°F (-5°C)24°F (-4°C)30°F (-1°C)40°F (5°C)51°F (10°C)60°F (16°C)68°F (20°C)70°F (21°C)63°F (17°C)52°F (11°C)40°F (5°C)29°F (-1°C)
Rainfall2.4 in (61 mm)2.2 in (56 mm)4.4 in (111 mm)5.1 in (129 mm)5.9 in (150 mm)7.1 in (181 mm)9.4 in (239 mm)7.7 in (197 mm)9 in (230 mm)7.2 in (183 mm)3.4 in (87 mm)2.4 in (60 mm)
Rainy days991313141721191714910
Snowfall9.9 in (25.2 cm)8 in (20.2 cm)6.3 in (15.9 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 cm)0.3 in (0.8 cm)3.8 in (9.6 cm)
Sunshine256 h241 h272 h274 h282 h235 h235 h270 h220 h227 h219 h235 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

Too few hot days today to project a reliable change

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.1°F (+1.2°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.9°F (+1.6°C)
  • May: +2.3°F (+1.3°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.0°F (+1.1°C)
  • August: +2.6°F (+1.4°C)
  • September: +3.0°F (+1.7°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.6°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.