ClimateSearch

Ebetsu, Hokkaido

Japan · 134k people · 13 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)31°F (-1°C)38°F (4°C)51°F (11°C)62°F (17°C)69°F (21°C)76°F (24°C)78°F (25°C)72°F (22°C)61°F (16°C)47°F (8°C)34°F (1°C)
Average low14°F (-10°C)16°F (-9°C)24°F (-4°C)35°F (2°C)45°F (7°C)54°F (12°C)62°F (17°C)64°F (18°C)56°F (13°C)43°F (6°C)32°F (0°C)20°F (-6°C)
Dew point14°F (-10°C)15°F (-10°C)22°F (-6°C)32°F (0°C)44°F (7°C)54°F (12°C)62°F (17°C)64°F (18°C)56°F (14°C)44°F (6°C)31°F (-1°C)19°F (-7°C)
Rainfall3.7 in (95 mm)3 in (75 mm)2.5 in (64 mm)2.6 in (66 mm)2.7 in (69 mm)2.9 in (73 mm)5 in (127 mm)5.8 in (147 mm)5.3 in (133 mm)3.8 in (97 mm)4.2 in (107 mm)5 in (126 mm)
Rainy days11109101089910111313
Snowfall12.6 in (31.9 cm)11.1 in (28.2 cm)10 in (25.4 cm)2.6 in (6.7 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.6 cm)4.2 in (10.7 cm)13.9 in (35.4 cm)
Sunshine134 h145 h184 h191 h180 h168 h155 h149 h151 h170 h132 h124 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

+2.7°F (+1.5°C)

Models range from +1.9°F (+1.1°C) to +3.1°F (+1.7°C)

Days above 90°F (32°C) a year

0 → 0

Warming by month
  • January: +2.6°F (+1.5°C)
  • February: +2.9°F (+1.6°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.7°F (+1.5°C)
  • May: +2.1°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.7°F (+1.5°C)
  • August: +3.1°F (+1.7°C)
  • September: +3.4°F (+1.9°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.7°F (+1.5°C)
  • December: +2.5°F (+1.4°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.