ClimateSearch

Qingyuan, Guangdong

China · 1.7M 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 high63°F (17°C)65°F (19°C)70°F (21°C)78°F (26°C)85°F (30°C)89°F (32°C)92°F (33°C)92°F (33°C)89°F (32°C)84°F (29°C)76°F (25°C)67°F (20°C)
Average low49°F (9°C)51°F (11°C)58°F (14°C)66°F (19°C)72°F (22°C)76°F (25°C)78°F (25°C)77°F (25°C)74°F (24°C)68°F (20°C)59°F (15°C)50°F (10°C)
Dew point46°F (8°C)51°F (11°C)58°F (14°C)66°F (19°C)72°F (22°C)76°F (25°C)77°F (25°C)77°F (25°C)73°F (23°C)64°F (18°C)55°F (13°C)46°F (8°C)
Rainfall1.8 in (45 mm)2.6 in (65 mm)4.3 in (108 mm)6.5 in (165 mm)8.7 in (222 mm)11.8 in (299 mm)7 in (179 mm)8.5 in (215 mm)4.4 in (112 mm)1.8 in (45 mm)1.7 in (43 mm)1.4 in (36 mm)
Rainy days7101212151712148355
Snowfall0 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 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine118 h74 h56 h74 h95 h96 h149 h159 h180 h210 h172 h164 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

+1.6°F (+0.9°C)

Models range from +1.1°F (+0.6°C) to +1.9°F (+1.0°C)

Days above 90°F (32°C) a year

30 → 61

About 2.1× as many

Warming by month
  • January: +2.7°F (+1.5°C)
  • February: +2.2°F (+1.2°C)
  • March: +2.2°F (+1.2°C)
  • April: +2.6°F (+1.4°C)
  • May: +2.3°F (+1.3°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.2°F (+0.7°C)
  • September: +1.7°F (+0.9°C)
  • October: +2.3°F (+1.3°C)
  • November: +2.4°F (+1.3°C)
  • December: +2.7°F (+1.5°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.