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 high49°F (9°C)50°F (10°C)56°F (14°C)66°F (19°C)73°F (23°C)77°F (25°C)84°F (29°C)87°F (31°C)80°F (27°C)71°F (22°C)62°F (17°C)53°F (12°C)
Average low31°F (0°C)33°F (1°C)39°F (4°C)48°F (9°C)57°F (14°C)65°F (18°C)72°F (22°C)74°F (23°C)67°F (20°C)56°F (14°C)45°F (7°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)
Rainfall1.6 in (40 mm)2 in (50 mm)3.4 in (87 mm)4.1 in (104 mm)4.8 in (122 mm)5.8 in (147 mm)6 in (152 mm)5.2 in (132 mm)7 in (177 mm)8 in (204 mm)2.9 in (73 mm)1.9 in (49 mm)
Rainy days561010101097101186
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)
Sunshine195 h169 h172 h166 h152 h101 h123 h169 h128 h132 h147 h174 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.