ClimateSearch

Bunkyo, Kanagawa

Japan · 240k people · 98 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)52°F (11°C)57°F (14°C)66°F (19°C)74°F (23°C)78°F (26°C)85°F (29°C)87°F (31°C)81°F (27°C)71°F (22°C)62°F (17°C)54°F (12°C)
Average low33°F (0°C)34°F (1°C)40°F (4°C)48°F (9°C)57°F (14°C)64°F (18°C)71°F (22°C)73°F (23°C)67°F (20°C)57°F (14°C)46°F (8°C)36°F (2°C)
Dew point28°F (-2°C)29°F (-2°C)36°F (2°C)46°F (8°C)55°F (13°C)64°F (18°C)71°F (22°C)72°F (22°C)66°F (19°C)55°F (13°C)45°F (7°C)34°F (1°C)
Rainfall2.2 in (55 mm)2.3 in (59 mm)4.1 in (105 mm)4.7 in (119 mm)5.8 in (148 mm)7.5 in (191 mm)6.4 in (164 mm)6.6 in (167 mm)7.8 in (199 mm)8.9 in (227 mm)3.3 in (84 mm)2.5 in (64 mm)
Rainy days6711111111108111197
Snowfall3.4 in (8.7 cm)4.1 in (10.4 cm)1.9 in (4.8 cm)0.1 in (0.2 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)0.5 in (1.3 cm)
Sunshine184 h160 h160 h162 h153 h104 h139 h186 h139 h136 h144 h166 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 +1.9°F (+1.0°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +2.4°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: +2.3°F (+1.3°C)
  • August: +2.3°F (+1.3°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.5°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.