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)66°F (19°C)71°F (22°C)78°F (26°C)83°F (29°C)86°F (30°C)88°F (31°C)89°F (31°C)86°F (30°C)82°F (28°C)74°F (24°C)66°F (19°C)
Average low49°F (10°C)53°F (12°C)59°F (15°C)66°F (19°C)72°F (22°C)76°F (25°C)77°F (25°C)77°F (25°C)74°F (24°C)68°F (20°C)60°F (15°C)51°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)
Rainfall3.2 in (80 mm)4.4 in (113 mm)8.9 in (226 mm)12.6 in (320 mm)15.6 in (398 mm)17.3 in (441 mm)11 in (279 mm)11 in (278 mm)6.3 in (161 mm)2.4 in (60 mm)2.4 in (60 mm)2.2 in (55 mm)
Rainy days101320202325232215777
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)
Sunshine195 h145 h131 h165 h210 h225 h289 h285 h276 h288 h239 h230 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.