ClimateSearch

Longgang, Guangdong

China · 215k people · 40 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)87°F (30°C)87°F (30°C)85°F (30°C)81°F (27°C)76°F (24°C)68°F (20°C)
Average low52°F (11°C)56°F (13°C)61°F (16°C)68°F (20°C)74°F (23°C)78°F (25°C)79°F (26°C)78°F (26°C)76°F (24°C)70°F (21°C)63°F (17°C)54°F (12°C)
Dew point49°F (9°C)53°F (12°C)60°F (16°C)67°F (20°C)73°F (23°C)77°F (25°C)78°F (25°C)78°F (25°C)74°F (24°C)67°F (19°C)59°F (15°C)49°F (10°C)
Rainfall1.2 in (30 mm)1.6 in (40 mm)3.3 in (84 mm)5.9 in (149 mm)10.9 in (277 mm)14.3 in (363 mm)10.3 in (262 mm)13.3 in (339 mm)8.3 in (210 mm)2.3 in (59 mm)1.4 in (34 mm)1.3 in (32 mm)
Rainy days5711152124242517754
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 h196 h212 h228 h250 h251 h313 h284 h282 h300 h256 h246 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

11 23

About 2.1× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.3°F (+1.3°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +1.7°F (+0.9°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.1°F (+0.6°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.5°F (+0.9°C)
  • November: +2.1°F (+1.2°C)
  • December: +2.1°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.