ClimateSearch

Wong Tai Sin, Wong Tai Sin District

Hong Kong · 425k people · 304 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 high63°F (17°C)64°F (18°C)69°F (20°C)75°F (24°C)81°F (27°C)84°F (29°C)86°F (30°C)86°F (30°C)84°F (29°C)80°F (27°C)74°F (23°C)66°F (19°C)
Average low52°F (11°C)54°F (12°C)59°F (15°C)65°F (18°C)72°F (22°C)75°F (24°C)76°F (25°C)76°F (24°C)74°F (23°C)69°F (21°C)62°F (17°C)55°F (13°C)
Dew point48°F (9°C)52°F (11°C)59°F (15°C)65°F (18°C)71°F (22°C)74°F (23°C)75°F (24°C)75°F (24°C)72°F (22°C)64°F (18°C)57°F (14°C)48°F (9°C)
Rainfall1 in (25 mm)1.5 in (39 mm)2.6 in (67 mm)5.5 in (139 mm)9.5 in (241 mm)14.6 in (371 mm)12.7 in (321 mm)15.7 in (399 mm)9.6 in (245 mm)3.3 in (83 mm)1.4 in (37 mm)1.2 in (30 mm)
Rainy days35691418171813544
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)
Sunshine168 h115 h121 h133 h139 h123 h177 h161 h184 h218 h187 h178 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

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.1°F (+1.2°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°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: +1.3°F (+0.7°C)
  • October: +1.7°F (+0.9°C)
  • November: +2.0°F (+1.1°C)
  • December: +2.0°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.