ClimateSearch

Asahikawa, Hokkaido

Japan · 334k people · 115 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 high23°F (-5°C)25°F (-4°C)33°F (1°C)46°F (8°C)61°F (16°C)69°F (21°C)75°F (24°C)76°F (24°C)68°F (20°C)56°F (13°C)40°F (5°C)27°F (-3°C)
Average low11°F (-12°C)12°F (-11°C)19°F (-7°C)30°F (-1°C)42°F (6°C)53°F (11°C)61°F (16°C)62°F (17°C)53°F (12°C)40°F (5°C)27°F (-3°C)14°F (-10°C)
Dew point12°F (-11°C)13°F (-11°C)20°F (-7°C)30°F (-1°C)43°F (6°C)53°F (12°C)62°F (16°C)63°F (17°C)54°F (12°C)41°F (5°C)29°F (-2°C)16°F (-9°C)
Rainfall2.3 in (59 mm)2.1 in (52 mm)2.7 in (68 mm)3 in (76 mm)3.6 in (92 mm)3.6 in (92 mm)5.9 in (149 mm)6.6 in (168 mm)5.7 in (146 mm)4.6 in (116 mm)4.3 in (109 mm)3.4 in (85 mm)
Rainy days161415141313151515161818
Snowfall19.2 in (48.8 cm)16.5 in (41.8 cm)15.9 in (40.4 cm)6.3 in (15.9 cm)0.4 in (1.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)1.5 in (3.9 cm)13.5 in (34.2 cm)23 in (58.3 cm)
Sunshine196 h214 h272 h278 h295 h285 h278 h261 h247 h241 h187 h181 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 +1.7°F (+1.0°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.8°F (+1.6°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.3°F (+1.3°C)
  • June: +1.7°F (+1.0°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.9°F (+1.6°C)
  • September: +3.2°F (+1.8°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.6°F (+1.4°C)
  • December: +2.4°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.