ClimateSearch

Shaoxing, Zhejiang

China · 2.3M people · 7 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)53°F (12°C)61°F (16°C)71°F (22°C)79°F (26°C)84°F (29°C)92°F (33°C)91°F (33°C)83°F (28°C)74°F (23°C)64°F (18°C)53°F (12°C)
Average low35°F (2°C)38°F (3°C)44°F (7°C)53°F (12°C)63°F (17°C)70°F (21°C)78°F (26°C)78°F (25°C)70°F (21°C)60°F (15°C)49°F (10°C)38°F (3°C)
Dew point34°F (1°C)37°F (3°C)44°F (7°C)53°F (12°C)62°F (17°C)70°F (21°C)75°F (24°C)75°F (24°C)68°F (20°C)58°F (14°C)48°F (9°C)37°F (3°C)
Rainfall3.3 in (83 mm)3.1 in (78 mm)5 in (127 mm)5.5 in (140 mm)6.7 in (171 mm)12.3 in (311 mm)7.2 in (182 mm)6.5 in (166 mm)4.5 in (115 mm)2.6 in (67 mm)2.8 in (70 mm)2.5 in (63 mm)
Rainy days111114131317141712798
Snowfall2.7 in (6.8 cm)1.7 in (4.2 cm)0.2 in (0.6 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 in (0 cm)0 in (0 cm)1.1 in (2.8 cm)
Sunshine180 h172 h194 h219 h246 h217 h303 h291 h242 h234 h188 h202 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

+2.1°F (+1.2°C)

Models range from +1.3°F (+0.7°C) to +2.6°F (+1.4°C)

Days above 90°F (32°C) a year

50 72

About 1.4× as many

Warming by month
  • January: +3.2°F (+1.8°C)
  • February: +2.3°F (+1.3°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.6°F (+1.4°C)
  • May: +1.5°F (+0.9°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.9°F (+1.1°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.9°F (+1.6°C)
  • October: +3.0°F (+1.7°C)
  • November: +2.8°F (+1.6°C)
  • December: +3.3°F (+1.8°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.