ClimateSearch

Santo António, Guangdong

China · 130k people · 18 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 high65°F (19°C)66°F (19°C)71°F (22°C)78°F (25°C)84°F (29°C)88°F (31°C)90°F (32°C)89°F (32°C)88°F (31°C)83°F (28°C)76°F (25°C)69°F (20°C)
Average low55°F (13°C)57°F (14°C)62°F (17°C)69°F (21°C)75°F (24°C)79°F (26°C)80°F (26°C)79°F (26°C)78°F (25°C)73°F (23°C)65°F (18°C)57°F (14°C)
Dew point52°F (11°C)56°F (13°C)62°F (17°C)69°F (21°C)74°F (23°C)77°F (25°C)78°F (25°C)78°F (25°C)75°F (24°C)68°F (20°C)61°F (16°C)52°F (11°C)
Rainfall1.1 in (28 mm)1.7 in (42 mm)2.8 in (72 mm)6.2 in (158 mm)10 in (254 mm)12.9 in (326 mm)11.4 in (288 mm)13.5 in (344 mm)7.1 in (182 mm)2.8 in (72 mm)1.3 in (34 mm)1.1 in (29 mm)
Rainy days45691316151610433
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)
Sunshine162 h114 h123 h142 h148 h132 h183 h165 h183 h218 h188 h176 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

+1.3°F (+0.7°C)

Models range from +0.6°F (+0.3°C) to +2.1°F (+1.2°C)

Days above 90°F (32°C) a year

3 → 5

About 1.7× as many

Warming by month
  • January: +2.2°F (+1.2°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +1.6°F (+0.9°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.9°F (+1.1°C)
  • November: +1.9°F (+1.1°C)
  • December: +2.0°F (+1.1°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.