ClimateSearch

Guangzhou, Guangdong

China · 16.1M people · 15 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 (18°C)66°F (19°C)71°F (22°C)79°F (26°C)85°F (30°C)89°F (32°C)91°F (33°C)91°F (33°C)89°F (32°C)84°F (29°C)77°F (25°C)69°F (20°C)
Average low51°F (10°C)54°F (12°C)60°F (15°C)67°F (19°C)73°F (23°C)77°F (25°C)78°F (26°C)78°F (25°C)75°F (24°C)70°F (21°C)62°F (16°C)53°F (12°C)
Dew point47°F (8°C)52°F (11°C)59°F (15°C)67°F (19°C)73°F (23°C)76°F (25°C)77°F (25°C)77°F (25°C)74°F (23°C)65°F (18°C)56°F (13°C)47°F (8°C)
Rainfall1.9 in (47 mm)2.1 in (52 mm)3.4 in (86 mm)6.2 in (157 mm)8.5 in (215 mm)11.5 in (293 mm)8.8 in (224 mm)8.6 in (219 mm)5.3 in (136 mm)2.3 in (58 mm)1.5 in (37 mm)1.6 in (42 mm)
Rainy days67910151714159445
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)
Sunshine135 h88 h78 h93 h114 h115 h166 h158 h175 h209 h177 h165 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

+1.4°F (+0.8°C)

Models range from +1.1°F (+0.6°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

41 → 68

About 1.7× as many

Warming by month
  • January: +2.6°F (+1.5°C)
  • February: +2.1°F (+1.2°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.9°F (+1.1°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.4°F (+1.4°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.