ClimateSearch

Ma On Shan, Sha Tin

Hong Kong · 215k people · 223 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 high64°F (18°C)66°F (19°C)71°F (22°C)76°F (24°C)80°F (27°C)83°F (28°C)84°F (29°C)84°F (29°C)83°F (28°C)79°F (26°C)73°F (23°C)66°F (19°C)
Average low54°F (12°C)56°F (14°C)62°F (16°C)68°F (20°C)73°F (23°C)76°F (25°C)77°F (25°C)77°F (25°C)75°F (24°C)71°F (21°C)64°F (18°C)56°F (13°C)
Dew point49°F (9°C)53°F (12°C)60°F (15°C)66°F (19°C)72°F (22°C)75°F (24°C)76°F (24°C)76°F (24°C)73°F (23°C)65°F (19°C)58°F (15°C)49°F (10°C)
Rainfall1 in (25 mm)1.4 in (35 mm)2.9 in (73 mm)5 in (127 mm)9.2 in (233 mm)12.9 in (328 mm)9.9 in (252 mm)12.7 in (324 mm)8.6 in (218 mm)2.8 in (72 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 h202 h226 h247 h269 h262 h320 h292 h287 h303 h261 h251 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: +2.3°F (+1.3°C)
  • February: +2.1°F (+1.1°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.1°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: +1.2°F (+0.7°C)
  • October: +1.6°F (+0.9°C)
  • November: +2.0°F (+1.1°C)
  • December: +1.9°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.