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)65°F (18°C)69°F (21°C)74°F (24°C)79°F (26°C)82°F (28°C)83°F (28°C)83°F (28°C)82°F (28°C)78°F (25°C)72°F (22°C)65°F (18°C)
Average low53°F (12°C)56°F (13°C)61°F (16°C)67°F (19°C)72°F (22°C)75°F (24°C)76°F (25°C)76°F (24°C)74°F (23°C)70°F (21°C)63°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 (24 mm)1.4 in (34 mm)2.8 in (71 mm)5 in (127 mm)9.2 in (233 mm)13.1 in (332 mm)9.9 in (253 mm)12.8 in (326 mm)8.5 in (217 mm)2.8 in (70 mm)1.4 in (35 mm)1.1 in (29 mm)
Rainy days4710152024232417754
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)
Sunshine249 h203 h228 h248 h270 h263 h322 h292 h288 h304 h261 h250 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.