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)79°F (26°C)85°F (30°C)88°F (31°C)90°F (32°C)90°F (32°C)89°F (32°C)84°F (29°C)78°F (25°C)70°F (21°C)
Average low52°F (11°C)55°F (13°C)60°F (16°C)67°F (20°C)74°F (23°C)78°F (25°C)79°F (26°C)78°F (26°C)76°F (25°C)71°F (22°C)63°F (17°C)55°F (13°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 (42 mm)2.9 in (73 mm)5.4 in (136 mm)8.6 in (217 mm)13.8 in (350 mm)12.2 in (310 mm)13.7 in (349 mm)9 in (228 mm)2.5 in (64 mm)1.8 in (47 mm)1.1 in (29 mm)
Rainy days45791318171812444
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)
Sunshine163 h111 h109 h117 h123 h114 h168 h153 h178 h215 h184 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

+1.4°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.