ClimateSearch

Ōtsu, Shiga

Japan · 345k people · 128 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 high45°F (7°C)46°F (8°C)53°F (12°C)63°F (17°C)72°F (22°C)78°F (26°C)84°F (29°C)87°F (31°C)80°F (26°C)69°F (21°C)59°F (15°C)49°F (10°C)
Average low31°F (0°C)31°F (0°C)36°F (2°C)45°F (7°C)55°F (13°C)63°F (17°C)71°F (22°C)73°F (23°C)66°F (19°C)55°F (13°C)44°F (7°C)35°F (2°C)
Dew point30°F (-1°C)30°F (-1°C)36°F (2°C)45°F (7°C)54°F (12°C)63°F (17°C)71°F (22°C)72°F (22°C)65°F (19°C)55°F (13°C)45°F (7°C)35°F (2°C)
Rainfall2.5 in (64 mm)2.9 in (73 mm)4.8 in (122 mm)5.2 in (133 mm)6.2 in (156 mm)8.3 in (211 mm)9.4 in (240 mm)5.4 in (138 mm)7.4 in (188 mm)6.5 in (166 mm)3.3 in (85 mm)2.6 in (66 mm)
Rainy days89131212151713131088
Snowfall2.2 in (5.6 cm)2.9 in (7.4 cm)0.7 in (1.7 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)0.8 in (2.1 cm)
Sunshine242 h227 h267 h267 h293 h255 h294 h330 h261 h252 h230 h235 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 +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

12 41

About 3.4× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.7°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.