ClimateSearch

Kusatsu, Shiga

Japan · 144k people · 105 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)49°F (9°C)56°F (13°C)66°F (19°C)75°F (24°C)81°F (27°C)88°F (31°C)91°F (33°C)83°F (28°C)73°F (23°C)62°F (17°C)52°F (11°C)
Average low33°F (0°C)33°F (1°C)38°F (3°C)47°F (8°C)57°F (14°C)65°F (18°C)73°F (23°C)75°F (24°C)67°F (20°C)56°F (14°C)45°F (7°C)37°F (3°C)
Dew point31°F (-1°C)31°F (-1°C)36°F (2°C)45°F (7°C)55°F (13°C)63°F (17°C)71°F (22°C)72°F (22°C)66°F (19°C)55°F (13°C)45°F (7°C)35°F (2°C)
Rainfall3.1 in (80 mm)2.9 in (74 mm)4.4 in (111 mm)5 in (128 mm)5.6 in (142 mm)7.3 in (186 mm)7.7 in (195 mm)5.1 in (129 mm)7.2 in (184 mm)6.2 in (156 mm)3 in (77 mm)2.9 in (73 mm)
Rainy days8811109111079877
Snowfall2.2 in (5.6 cm)2.8 in (7.1 cm)0.5 in (1.3 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)0.9 in (2.3 cm)
Sunshine157 h143 h165 h161 h164 h120 h153 h205 h155 h162 h153 h157 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 (+1.5°C)

Days above 90°F (32°C) a year

14 → 45

About 3.2× 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: +2.6°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.