ClimateSearch

Shaoyang, Hunan

China · 753k people · 242 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)60°F (16°C)72°F (22°C)80°F (27°C)85°F (30°C)92°F (33°C)90°F (32°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)57°F (14°C)65°F (18°C)72°F (22°C)76°F (25°C)75°F (24°C)68°F (20°C)59°F (15°C)49°F (10°C)40°F (4°C)
Dew point35°F (1°C)39°F (4°C)47°F (8°C)57°F (14°C)65°F (18°C)72°F (22°C)74°F (24°C)73°F (23°C)66°F (19°C)56°F (14°C)47°F (8°C)37°F (3°C)
Rainfall2.1 in (54 mm)2.8 in (72 mm)4.1 in (104 mm)6.1 in (155 mm)7.3 in (184 mm)7.2 in (184 mm)4.8 in (121 mm)3.8 in (98 mm)2.5 in (64 mm)2.5 in (64 mm)3.1 in (79 mm)2 in (50 mm)
Rainy days91115141312886687
Snowfall2.2 in (5.6 cm)0.9 in (2.3 cm)0.3 in (0.7 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)0.8 in (2.1 cm)
Sunshine80 h66 h68 h93 h116 h109 h167 h178 h145 h133 h115 h112 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 +1.1°F (+0.6°C) to +2.4°F (+1.4°C)

Days above 90°F (32°C) a year

36 → 59

About 1.7× as many

Warming by month
  • January: +3.3°F (+1.8°C)
  • February: +2.4°F (+1.4°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.9°F (+1.6°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.7°F (+0.9°C)
  • September: +1.8°F (+1.0°C)
  • October: +2.0°F (+1.1°C)
  • November: +2.4°F (+1.3°C)
  • December: +2.8°F (+1.6°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.