ClimateSearch

Shaoshan, Hunan

China · 118k people · 108 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)72°F (22°C)80°F (27°C)86°F (30°C)93°F (34°C)91°F (33°C)84°F (29°C)74°F (23°C)64°F (18°C)53°F (12°C)
Average low37°F (3°C)41°F (5°C)48°F (9°C)58°F (14°C)66°F (19°C)73°F (23°C)78°F (26°C)77°F (25°C)69°F (21°C)60°F (15°C)49°F (10°C)40°F (4°C)
Dew point34°F (1°C)39°F (4°C)47°F (8°C)57°F (14°C)65°F (18°C)72°F (22°C)75°F (24°C)74°F (23°C)67°F (19°C)56°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.3 in (60 mm)3.2 in (81 mm)5.2 in (131 mm)6.5 in (166 mm)7.1 in (180 mm)7.2 in (183 mm)4.7 in (120 mm)3.5 in (89 mm)2.6 in (67 mm)2.4 in (60 mm)3.1 in (78 mm)2 in (51 mm)
Rainy days91115141211765687
Snowfall2 in (5.1 cm)0.9 in (2.2 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)0.7 in (1.9 cm)
Sunshine87 h73 h77 h97 h120 h115 h168 h181 h149 h141 h118 h118 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

+1.8°F (+1.0°C)

Models range from +1.2°F (+0.7°C) to +2.4°F (+1.3°C)

Days above 90°F (32°C) a year

42 → 64

About 1.5× as many

Warming by month
  • January: +3.4°F (+1.9°C)
  • February: +2.7°F (+1.5°C)
  • March: +2.4°F (+1.3°C)
  • April: +2.8°F (+1.6°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.6°F (+0.9°C)
  • September: +2.0°F (+1.1°C)
  • October: +2.3°F (+1.3°C)
  • November: +2.6°F (+1.4°C)
  • December: +3.2°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.