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 high46°F (8°C)48°F (9°C)55°F (13°C)65°F (18°C)74°F (23°C)80°F (26°C)87°F (31°C)90°F (32°C)82°F (28°C)71°F (22°C)62°F (16°C)51°F (11°C)
Average low34°F (1°C)34°F (1°C)38°F (4°C)47°F (9°C)57°F (14°C)65°F (18°C)73°F (23°C)75°F (24°C)68°F (20°C)57°F (14°C)47°F (8°C)38°F (3°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)
Rainfall3 in (76 mm)2.9 in (73 mm)4.4 in (112 mm)5.1 in (129 mm)5.6 in (142 mm)7.2 in (184 mm)7.7 in (195 mm)5.1 in (131 mm)7.2 in (183 mm)6.1 in (154 mm)3 in (76 mm)2.7 in (68 mm)
Rainy days78111010111189977
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)
Sunshine161 h146 h168 h164 h170 h122 h155 h208 h159 h167 h158 h162 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.