ClimateSearch

Kobe, Hyōgo

Japan · 1.5M people · 36 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 high47°F (8°C)48°F (9°C)55°F (13°C)64°F (18°C)72°F (22°C)78°F (26°C)84°F (29°C)87°F (30°C)81°F (27°C)71°F (22°C)61°F (16°C)51°F (11°C)
Average low36°F (2°C)35°F (2°C)40°F (5°C)49°F (10°C)59°F (15°C)67°F (19°C)75°F (24°C)77°F (25°C)70°F (21°C)60°F (15°C)49°F (10°C)40°F (5°C)
Dew point33°F (0°C)33°F (1°C)38°F (3°C)47°F (9°C)57°F (14°C)66°F (19°C)73°F (23°C)74°F (23°C)67°F (20°C)57°F (14°C)47°F (8°C)38°F (3°C)
Rainfall2.2 in (56 mm)2.6 in (67 mm)4.4 in (113 mm)5 in (127 mm)5.9 in (151 mm)7.9 in (201 mm)8.4 in (213 mm)5.1 in (130 mm)7.6 in (194 mm)6.5 in (164 mm)3.4 in (86 mm)2.6 in (67 mm)
Rainy days68111011141514131077
Snowfall0.5 in (1.2 cm)1.3 in (3.2 cm)0.1 in (0.3 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 in (0 cm)0 in (0 cm)0.2 in (0.4 cm)
Sunshine247 h234 h272 h271 h300 h259 h300 h333 h267 h254 h234 h242 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 +1.7°F (+1.0°C) to +2.8°F (+1.5°C)

Days above 90°F (32°C) a year

7 23

About 3.4× as many

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.1°F (+1.2°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.3°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.