ClimateSearch

Chūō, Tokyo

Japan · 169k people · 21 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 high50°F (10°C)51°F (10°C)56°F (14°C)66°F (19°C)73°F (23°C)78°F (25°C)85°F (29°C)88°F (31°C)81°F (27°C)71°F (22°C)62°F (17°C)54°F (12°C)
Average low36°F (2°C)37°F (3°C)42°F (6°C)50°F (10°C)59°F (15°C)66°F (19°C)73°F (23°C)75°F (24°C)69°F (21°C)59°F (15°C)49°F (9°C)40°F (4°C)
Dew point29°F (-1°C)30°F (-1°C)37°F (3°C)47°F (8°C)56°F (13°C)64°F (18°C)71°F (22°C)73°F (23°C)67°F (19°C)57°F (14°C)46°F (8°C)35°F (2°C)
Rainfall2.3 in (57 mm)2.3 in (59 mm)4.2 in (108 mm)4.6 in (117 mm)5.1 in (131 mm)6.4 in (162 mm)6.2 in (157 mm)5.3 in (134 mm)7.5 in (190 mm)8.3 in (212 mm)3.5 in (90 mm)2.4 in (60 mm)
Rainy days661111101097101096
Snowfall2.4 in (6.2 cm)2.9 in (7.4 cm)1.1 in (2.7 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)0.1 in (0.2 cm)0.3 in (0.8 cm)
Sunshine188 h164 h166 h165 h154 h105 h135 h184 h135 h135 h143 h167 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 +1.8°F (+1.0°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

7 → 15

About 2.1× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.4°F (+1.4°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.9°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.1°F (+1.1°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.