ClimateSearch

Kokubunji, Tokyo

Japan · 129k people · 82 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)47°F (8°C)53°F (12°C)62°F (17°C)70°F (21°C)75°F (24°C)82°F (28°C)84°F (29°C)78°F (25°C)68°F (20°C)59°F (15°C)50°F (10°C)
Average low29°F (-2°C)30°F (-1°C)37°F (3°C)46°F (8°C)55°F (13°C)63°F (17°C)71°F (21°C)73°F (23°C)67°F (19°C)56°F (13°C)45°F (7°C)35°F (1°C)
Dew point27°F (-3°C)28°F (-2°C)35°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)44°F (7°C)33°F (1°C)
Rainfall2.7 in (69 mm)2.6 in (66 mm)4.8 in (122 mm)4.9 in (124 mm)5.6 in (142 mm)7.2 in (182 mm)7.3 in (185 mm)5.8 in (147 mm)8.3 in (210 mm)8.7 in (220 mm)3.6 in (91 mm)2.4 in (62 mm)
Rainy days781313131617151514107
Snowfall4.5 in (11.5 cm)4.7 in (12 cm)2.5 in (6.4 cm)0.2 in (0.5 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 (0.3 cm)0.7 in (1.9 cm)
Sunshine256 h237 h260 h268 h275 h225 h259 h296 h235 h223 h216 h234 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 +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

5 10

About 2.2× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.5°F (+1.4°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.7°F (+1.5°C)
  • October: +2.6°F (+1.4°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.1°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.