ClimateSearch

Zhaoqing, Guangdong

China · 1.6M 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 (18°C)67°F (19°C)71°F (22°C)79°F (26°C)86°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)68°F (20°C)
Average low51°F (11°C)54°F (12°C)60°F (16°C)67°F (20°C)73°F (23°C)77°F (25°C)78°F (26°C)78°F (25°C)76°F (24°C)70°F (21°C)62°F (17°C)53°F (12°C)
Dew point47°F (9°C)52°F (11°C)59°F (15°C)67°F (20°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 (14°C)47°F (9°C)
Rainfall1.7 in (44 mm)2 in (50 mm)3.9 in (98 mm)6.4 in (162 mm)9.9 in (252 mm)11.5 in (292 mm)8.7 in (220 mm)10.3 in (262 mm)5.9 in (149 mm)2.1 in (54 mm)1.5 in (39 mm)1.6 in (40 mm)
Rainy days5810111518141610445
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)
Sunshine117 h74 h63 h83 h106 h109 h153 h153 h170 h201 h170 h158 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 +1.1°F (+0.6°C) to +1.8°F (+1.0°C)

Days above 90°F (32°C) a year

31 → 56

About 1.8× as many

Warming by month
  • January: +2.4°F (+1.4°C)
  • February: +1.9°F (+1.1°C)
  • March: +2.0°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.1°F (+1.2°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.3°F (+0.7°C)
  • August: +1.0°F (+0.5°C)
  • September: +1.5°F (+0.8°C)
  • October: +2.1°F (+1.2°C)
  • November: +2.1°F (+1.2°C)
  • December: +2.4°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.