ClimateSearch

Sandachō, Hyōgo

Japan · 133k people · 149 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 high46°F (8°C)48°F (9°C)55°F (13°C)65°F (19°C)74°F (23°C)79°F (26°C)86°F (30°C)89°F (32°C)81°F (27°C)71°F (22°C)61°F (16°C)51°F (11°C)
Average low32°F (0°C)33°F (0°C)38°F (3°C)47°F (8°C)56°F (14°C)65°F (18°C)73°F (23°C)75°F (24°C)67°F (20°C)56°F (13°C)45°F (7°C)36°F (2°C)
Dew point30°F (-1°C)31°F (-1°C)36°F (2°C)45°F (7°C)55°F (13°C)64°F (18°C)72°F (22°C)73°F (23°C)66°F (19°C)55°F (13°C)45°F (7°C)35°F (2°C)
Rainfall2.3 in (58 mm)2.5 in (64 mm)4.1 in (105 mm)4.7 in (119 mm)5.2 in (133 mm)6.7 in (170 mm)6.5 in (165 mm)4 in (102 mm)6.7 in (171 mm)5.4 in (138 mm)2.8 in (72 mm)2.4 in (60 mm)
Rainy days67101010101069866
Snowfall1.6 in (4 cm)2.4 in (6.1 cm)0.6 in (1.5 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)0.7 in (1.9 cm)
Sunshine165 h150 h171 h168 h174 h125 h155 h208 h163 h172 h162 h165 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 +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°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: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.7°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.