ClimateSearch

Chaozhou, Guangdong

China · 1.8M people · 24 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 high66°F (19°C)68°F (20°C)73°F (23°C)78°F (26°C)83°F (28°C)85°F (30°C)88°F (31°C)87°F (31°C)86°F (30°C)83°F (28°C)77°F (25°C)69°F (20°C)
Average low49°F (10°C)52°F (11°C)57°F (14°C)64°F (18°C)71°F (22°C)76°F (24°C)77°F (25°C)77°F (25°C)74°F (23°C)67°F (20°C)60°F (15°C)51°F (11°C)
Dew point48°F (9°C)51°F (11°C)56°F (14°C)64°F (18°C)71°F (22°C)76°F (24°C)77°F (25°C)77°F (25°C)74°F (23°C)65°F (19°C)58°F (14°C)49°F (10°C)
Rainfall1.4 in (35 mm)2 in (51 mm)3.2 in (81 mm)5.2 in (132 mm)8.8 in (224 mm)11.7 in (297 mm)9.6 in (243 mm)12.5 in (316 mm)7.3 in (185 mm)2 in (52 mm)1.8 in (45 mm)1.5 in (39 mm)
Rainy days5812142023232417655
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)
Sunshine242 h192 h206 h219 h232 h244 h310 h282 h287 h290 h248 h240 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 +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

27 57

About 2.1× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.4°F (+1.3°C)
  • March: +2.1°F (+1.2°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.2°F (+1.2°C)
  • June: +2.0°F (+1.1°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.3°F (+0.7°C)
  • September: +1.6°F (+0.9°C)
  • October: +1.9°F (+1.1°C)
  • November: +2.3°F (+1.3°C)
  • December: +2.3°F (+1.3°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.