ClimateSearch

Tin Shui Wai, Yuen Long

Hong Kong · 286k people · 12 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)68°F (20°C)73°F (23°C)79°F (26°C)85°F (29°C)88°F (31°C)90°F (32°C)90°F (32°C)88°F (31°C)84°F (29°C)78°F (25°C)70°F (21°C)
Average low54°F (12°C)57°F (14°C)62°F (16°C)68°F (20°C)75°F (24°C)78°F (26°C)79°F (26°C)79°F (26°C)77°F (25°C)72°F (22°C)65°F (18°C)56°F (14°C)
Dew point50°F (10°C)55°F (13°C)61°F (16°C)68°F (20°C)74°F (23°C)77°F (25°C)78°F (25°C)78°F (25°C)74°F (24°C)67°F (19°C)59°F (15°C)50°F (10°C)
Rainfall1 in (25 mm)1.4 in (35 mm)2.5 in (63 mm)5.3 in (135 mm)8.1 in (205 mm)13.2 in (335 mm)11.7 in (297 mm)13.4 in (340 mm)8 in (202 mm)2.8 in (72 mm)1.4 in (36 mm)1 in (26 mm)
Rainy days45681217151610433
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)
Sunshine170 h119 h127 h139 h144 h128 h181 h164 h185 h220 h190 h179 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

9 → 18

About 2.0× as many

Warming by month
  • January: +2.4°F (+1.3°C)
  • February: +2.1°F (+1.2°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +1.7°F (+1.0°C)
  • July: +1.4°F (+0.8°C)
  • August: +1.0°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.