ClimateSearch

Tottori-shi, Tottori

Japan · 188k people · 8 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)66°F (19°C)74°F (24°C)80°F (27°C)87°F (30°C)90°F (32°C)81°F (27°C)72°F (22°C)62°F (17°C)52°F (11°C)
Average low34°F (1°C)34°F (1°C)38°F (3°C)46°F (8°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)37°F (3°C)
Dew point34°F (1°C)33°F (1°C)38°F (3°C)46°F (8°C)55°F (13°C)64°F (18°C)72°F (22°C)73°F (23°C)66°F (19°C)56°F (13°C)46°F (8°C)38°F (3°C)
Rainfall6.4 in (163 mm)5.3 in (135 mm)5.2 in (131 mm)4.3 in (110 mm)4.8 in (121 mm)5.4 in (138 mm)7.2 in (184 mm)4.7 in (120 mm)9.2 in (234 mm)6 in (151 mm)5.4 in (137 mm)6.9 in (176 mm)
Rainy days2117141110910711101419
Snowfall11.2 in (28.4 cm)9.4 in (23.8 cm)2.9 in (7.4 cm)0.1 in (0.2 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)0.1 in (0.2 cm)5.2 in (13.1 cm)
Sunshine128 h127 h157 h167 h180 h133 h155 h197 h146 h159 h138 h126 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 +2.0°F (+1.1°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: +2.1°F (+1.2°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.1°F (+1.2°C)
  • June: +2.3°F (+1.3°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.9°F (+1.6°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.4°F (+1.3°C)
  • December: +2.2°F (+1.2°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.