ClimateSearch

Odawara, Kanagawa

Japan · 189k people · 14 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 (9°C)54°F (12°C)61°F (16°C)68°F (20°C)73°F (23°C)79°F (26°C)82°F (28°C)77°F (25°C)68°F (20°C)60°F (16°C)52°F (11°C)
Average low36°F (2°C)36°F (2°C)41°F (5°C)49°F (10°C)58°F (14°C)65°F (18°C)72°F (22°C)74°F (23°C)69°F (21°C)60°F (15°C)50°F (10°C)41°F (5°C)
Dew point31°F (-1°C)32°F (0°C)38°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 (19°C)57°F (14°C)47°F (8°C)37°F (3°C)
Rainfall3.7 in (95 mm)4.2 in (107 mm)7.2 in (184 mm)6.9 in (176 mm)7.2 in (183 mm)9.7 in (246 mm)9.3 in (235 mm)7.2 in (182 mm)10.3 in (261 mm)9.8 in (250 mm)5.1 in (129 mm)3.5 in (90 mm)
Rainy days101116141417181616151210
Snowfall7.1 in (18 cm)8.1 in (20.7 cm)4.9 in (12.5 cm)0.6 in (1.4 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)0.2 in (0.6 cm)1.4 in (3.6 cm)
Sunshine256 h236 h265 h270 h283 h239 h284 h316 h253 h237 h220 h237 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 +2.4°F (+1.3°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 (+1.3°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.5°F (+1.4°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.