ClimateSearch

Kiryū, Gunma

Japan · 109k people · 107 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 high44°F (7°C)46°F (8°C)53°F (12°C)63°F (17°C)72°F (22°C)76°F (25°C)83°F (28°C)85°F (29°C)78°F (25°C)68°F (20°C)58°F (15°C)49°F (9°C)
Average low29°F (-2°C)29°F (-2°C)35°F (1°C)44°F (7°C)54°F (12°C)62°F (17°C)69°F (21°C)72°F (22°C)65°F (19°C)54°F (12°C)42°F (6°C)33°F (1°C)
Dew point25°F (-4°C)26°F (-4°C)32°F (0°C)42°F (6°C)53°F (11°C)62°F (17°C)70°F (21°C)71°F (22°C)65°F (18°C)54°F (12°C)42°F (5°C)31°F (-1°C)
Rainfall2 in (50 mm)2 in (50 mm)3.9 in (99 mm)4.3 in (110 mm)5.4 in (137 mm)7 in (178 mm)8.5 in (215 mm)6.9 in (174 mm)8.3 in (211 mm)6.7 in (170 mm)2.6 in (66 mm)1.8 in (45 mm)
Rainy days78121214192120171387
Snowfall7.1 in (18 cm)6.8 in (17.3 cm)5.6 in (14.2 cm)1.3 in (3.2 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)0.3 in (0.8 cm)2.6 in (6.5 cm)
Sunshine266 h249 h280 h284 h292 h247 h261 h294 h232 h238 h228 h245 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 +1.8°F (+1.0°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

10 18

About 1.9× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.2°F (+1.2°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.5°F (+1.4°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.4°F (+1.4°C)
  • December: +2.0°F (+1.1°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.