ClimateSearch

Qionghai, Hainan

China · 528k people · 25 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 high72°F (22°C)74°F (24°C)79°F (26°C)83°F (29°C)87°F (30°C)88°F (31°C)88°F (31°C)87°F (31°C)85°F (30°C)82°F (28°C)78°F (26°C)73°F (23°C)
Average low64°F (18°C)66°F (19°C)70°F (21°C)75°F (24°C)78°F (26°C)80°F (27°C)80°F (27°C)79°F (26°C)77°F (25°C)74°F (23°C)71°F (22°C)65°F (19°C)
Dew point61°F (16°C)64°F (18°C)69°F (20°C)73°F (23°C)76°F (25°C)78°F (25°C)77°F (25°C)77°F (25°C)76°F (24°C)72°F (22°C)67°F (20°C)62°F (17°C)
Rainfall1.1 in (29 mm)1.1 in (29 mm)1.7 in (44 mm)2.9 in (74 mm)6 in (152 mm)5.8 in (147 mm)7.3 in (185 mm)9.5 in (241 mm)9.7 in (248 mm)8.3 in (211 mm)2.8 in (71 mm)1.6 in (40 mm)
Rainy days781012171718242317128
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)
Sunshine221 h218 h290 h306 h328 h320 h330 h301 h268 h280 h245 h212 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

+1.6°F (+0.9°C)

Models range from +1.3°F (+0.7°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

22 43

About 2.0× as many

Warming by month
  • January: +1.5°F (+0.8°C)
  • February: +1.2°F (+0.7°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.5°F (+1.4°C)
  • May: +2.5°F (+1.4°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.5°F (+0.8°C)
  • August: +1.5°F (+0.8°C)
  • September: +1.5°F (+0.8°C)
  • October: +2.0°F (+1.1°C)
  • November: +1.8°F (+1.0°C)
  • December: +1.6°F (+0.9°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.