ClimateSearch

Chóngfú, Zhejiang

China · 112k people · 11 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)52°F (11°C)60°F (15°C)70°F (21°C)78°F (26°C)83°F (28°C)91°F (33°C)90°F (32°C)82°F (28°C)74°F (23°C)64°F (18°C)52°F (11°C)
Average low34°F (1°C)37°F (3°C)44°F (6°C)53°F (12°C)62°F (17°C)70°F (21°C)78°F (26°C)78°F (25°C)70°F (21°C)59°F (15°C)49°F (9°C)37°F (3°C)
Dew point32°F (0°C)36°F (2°C)42°F (6°C)52°F (11°C)61°F (16°C)70°F (21°C)76°F (24°C)75°F (24°C)68°F (20°C)57°F (14°C)47°F (8°C)36°F (2°C)
Rainfall3.1 in (79 mm)3.2 in (81 mm)5 in (127 mm)5.4 in (138 mm)6.1 in (156 mm)11.8 in (299 mm)7.2 in (182 mm)6.2 in (158 mm)3.8 in (96 mm)2.3 in (58 mm)2.6 in (67 mm)2.3 in (59 mm)
Rainy days111013121216141511687
Snowfall1.8 in (4.5 cm)1.1 in (2.9 cm)0.2 in (0.4 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 in (0 cm)0 in (0 cm)0.7 in (1.8 cm)
Sunshine187 h175 h201 h224 h253 h223 h297 h294 h250 h243 h196 h208 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 +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

42 68

About 1.6× as many

Warming by month
  • January: +3.2°F (+1.8°C)
  • February: +2.4°F (+1.4°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.7°F (+1.5°C)
  • May: +1.5°F (+0.8°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.1°F (+1.2°C)
  • August: +2.1°F (+1.2°C)
  • September: +3.0°F (+1.7°C)
  • October: +3.0°F (+1.7°C)
  • November: +2.9°F (+1.6°C)
  • December: +3.3°F (+1.9°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.