ClimateSearch

Tomakomai, Hokkaido

Japan · 175k people · 7 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 high29°F (-2°C)30°F (-1°C)36°F (2°C)46°F (8°C)55°F (13°C)62°F (17°C)69°F (21°C)73°F (23°C)68°F (20°C)58°F (14°C)45°F (7°C)33°F (1°C)
Average low18°F (-8°C)18°F (-8°C)25°F (-4°C)34°F (1°C)44°F (7°C)53°F (12°C)61°F (16°C)65°F (18°C)59°F (15°C)47°F (9°C)35°F (2°C)24°F (-4°C)
Dew point17°F (-8°C)17°F (-8°C)24°F (-4°C)33°F (1°C)44°F (7°C)53°F (12°C)62°F (16°C)65°F (18°C)58°F (14°C)45°F (7°C)32°F (0°C)21°F (-6°C)
Rainfall1.8 in (45 mm)1.7 in (44 mm)2.5 in (63 mm)3.1 in (78 mm)4.4 in (111 mm)4 in (102 mm)5.5 in (140 mm)7.7 in (195 mm)7 in (178 mm)4.6 in (116 mm)3.1 in (80 mm)2.5 in (63 mm)
Rainy days771111121214151512119
Snowfall12 in (30.5 cm)11.3 in (28.8 cm)11.5 in (29.2 cm)3.9 in (9.8 cm)0.2 in (0.5 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.4 in (0.9 cm)3.1 in (7.9 cm)11.1 in (28.2 cm)
Sunshine232 h241 h291 h300 h302 h302 h282 h271 h253 h262 h219 h219 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

+2.9°F (+1.6°C)

Models range from +2.3°F (+1.3°C) to +3.4°F (+1.9°C)

Days above 90°F (32°C) a year

0 0

Warming by month
  • January: +2.8°F (+1.5°C)
  • February: +2.9°F (+1.6°C)
  • March: +2.5°F (+1.4°C)
  • April: +2.8°F (+1.6°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.4°F (+1.4°C)
  • July: +3.1°F (+1.7°C)
  • August: +3.2°F (+1.8°C)
  • September: +3.4°F (+1.9°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.7°F (+1.5°C)
  • December: +2.6°F (+1.5°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.