ClimateSearch

Shaping, Guangdong

China · 108k people · 13 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)69°F (20°C)74°F (23°C)80°F (27°C)85°F (29°C)87°F (31°C)89°F (32°C)88°F (31°C)86°F (30°C)82°F (28°C)76°F (25°C)68°F (20°C)
Average low52°F (11°C)55°F (13°C)61°F (16°C)68°F (20°C)74°F (23°C)77°F (25°C)78°F (26°C)78°F (26°C)75°F (24°C)69°F (21°C)62°F (17°C)54°F (12°C)
Dew point47°F (9°C)52°F (11°C)60°F (15°C)67°F (20°C)73°F (23°C)76°F (25°C)77°F (25°C)77°F (25°C)73°F (23°C)65°F (18°C)56°F (14°C)47°F (8°C)
Rainfall1.4 in (36 mm)1.9 in (49 mm)4 in (101 mm)7.1 in (180 mm)10.7 in (271 mm)11.2 in (285 mm)8.7 in (221 mm)10.8 in (274 mm)7.6 in (193 mm)2.6 in (67 mm)1.4 in (34 mm)1.5 in (37 mm)
Rainy days6914162122212317765
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)
Sunshine208 h160 h163 h196 h238 h253 h306 h282 h271 h287 h244 h231 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 +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

34 60

About 1.8× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.4°F (+1.3°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.4°F (+0.8°C)
  • October: +2.0°F (+1.1°C)
  • November: +2.0°F (+1.1°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.