ClimateSearch

Noda, Chiba

Japan · 154k 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 high47°F (8°C)49°F (9°C)55°F (13°C)64°F (18°C)72°F (22°C)77°F (25°C)83°F (29°C)86°F (30°C)79°F (26°C)70°F (21°C)60°F (16°C)51°F (11°C)
Average low30°F (-1°C)31°F (0°C)38°F (3°C)47°F (8°C)56°F (14°C)64°F (18°C)71°F (22°C)74°F (23°C)68°F (20°C)57°F (14°C)46°F (8°C)35°F (2°C)
Dew point27°F (-3°C)28°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)56°F (13°C)45°F (7°C)33°F (1°C)
Rainfall2.3 in (57 mm)2.2 in (55 mm)4 in (103 mm)4.2 in (106 mm)5.1 in (130 mm)6.2 in (158 mm)6.4 in (161 mm)4.7 in (120 mm)7 in (178 mm)7.7 in (195 mm)3.2 in (82 mm)2.1 in (53 mm)
Rainy days67111112141513141397
Snowfall2.7 in (6.9 cm)3.1 in (7.8 cm)1.1 in (2.8 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 (0.2 cm)0.4 in (0.9 cm)
Sunshine256 h238 h261 h267 h272 h223 h251 h291 h229 h219 h212 h232 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 +2.0°F (+1.1°C) to +2.5°F (+1.4°C)

Days above 90°F (32°C) a year

12 32

About 2.6× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.4°F (+1.3°C)
  • March: +2.1°F (+1.1°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +2.3°F (+1.3°C)
  • August: +2.4°F (+1.3°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.5°F (+1.4°C)
  • November: +2.4°F (+1.4°C)
  • December: +2.0°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.