ClimateSearch

Tsu, Mie

Japan · 275k people · 4 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 high48°F (9°C)49°F (10°C)56°F (13°C)64°F (18°C)72°F (22°C)78°F (25°C)85°F (29°C)87°F (30°C)80°F (27°C)71°F (22°C)61°F (16°C)52°F (11°C)
Average low36°F (2°C)36°F (2°C)40°F (5°C)49°F (9°C)57°F (14°C)66°F (19°C)74°F (23°C)75°F (24°C)70°F (21°C)59°F (15°C)49°F (9°C)40°F (4°C)
Dew point32°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)74°F (23°C)68°F (20°C)57°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.7 in (68 mm)2.9 in (74 mm)5.1 in (129 mm)5.8 in (148 mm)6.9 in (174 mm)9.3 in (237 mm)8.6 in (220 mm)6.7 in (170 mm)10.1 in (257 mm)9.1 in (231 mm)4.2 in (107 mm)2.7 in (69 mm)
Rainy days78111112151716151287
Snowfall0.8 in (2.1 cm)1.7 in (4.3 cm)0.3 in (0.8 cm)0 in (0.1 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)0.3 in (0.7 cm)
Sunshine256 h240 h277 h273 h299 h260 h304 h332 h265 h251 h233 h246 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

+2.4°F (+1.3°C)

Models range from +1.8°F (+1.0°C) to +2.8°F (+1.6°C)

Days above 90°F (32°C) a year

12 38

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: +2.2°F (+1.2°C)
  • May: +1.7°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.6°F (+1.4°C)
  • August: +2.5°F (+1.4°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.6°F (+1.5°C)
  • November: +2.6°F (+1.4°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.