ClimateSearch

Tantou, Guangdong

China · 320k people · 7 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 high67°F (19°C)69°F (21°C)74°F (23°C)79°F (26°C)83°F (29°C)86°F (30°C)87°F (31°C)87°F (31°C)86°F (30°C)83°F (28°C)77°F (25°C)69°F (21°C)
Average low53°F (12°C)56°F (14°C)62°F (17°C)69°F (20°C)74°F (23°C)78°F (26°C)79°F (26°C)79°F (26°C)76°F (25°C)71°F (22°C)64°F (18°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)77°F (25°C)74°F (23°C)66°F (19°C)58°F (14°C)49°F (9°C)
Rainfall1.9 in (48 mm)2.6 in (67 mm)4.3 in (110 mm)6.3 in (160 mm)10.8 in (273 mm)13.8 in (352 mm)9.4 in (240 mm)12 in (305 mm)7.6 in (194 mm)2.2 in (56 mm)1.5 in (39 mm)1.6 in (42 mm)
Rainy days81014142023222315765
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)
Sunshine236 h192 h213 h232 h256 h257 h315 h287 h282 h298 h255 h244 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

14 26

About 1.9× as many

Warming by month
  • January: +2.5°F (+1.4°C)
  • February: +2.2°F (+1.2°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +1.5°F (+0.9°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.0°F (+0.5°C)
  • September: +1.2°F (+0.7°C)
  • October: +1.8°F (+1.0°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.1°F (+1.2°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.