ClimateSearch

Danshui, Taipei

Taiwan · 189k people · 19 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)65°F (18°C)69°F (21°C)75°F (24°C)81°F (27°C)85°F (29°C)87°F (31°C)87°F (30°C)83°F (29°C)78°F (25°C)73°F (23°C)67°F (19°C)
Average low56°F (14°C)56°F (14°C)60°F (15°C)65°F (19°C)72°F (22°C)76°F (25°C)79°F (26°C)78°F (26°C)76°F (24°C)72°F (22°C)67°F (19°C)60°F (16°C)
Dew point53°F (12°C)55°F (13°C)58°F (15°C)65°F (18°C)71°F (21°C)75°F (24°C)77°F (25°C)77°F (25°C)73°F (23°C)67°F (20°C)63°F (17°C)56°F (14°C)
Rainfall3.1 in (79 mm)3.8 in (97 mm)4.5 in (115 mm)5 in (127 mm)7 in (177 mm)7.3 in (185 mm)5 in (128 mm)7.8 in (197 mm)6.9 in (175 mm)5.2 in (131 mm)3.9 in (98 mm)3.3 in (84 mm)
Rainy days131315141515121514121313
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)
Sunshine152 h154 h214 h245 h270 h286 h353 h323 h292 h249 h188 h157 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

+1.8°F (+1.0°C)

Models range from +1.8°F (+1.0°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

9 27

About 3.1× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.4°F (+0.8°C)
  • April: +1.9°F (+1.1°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.6°F (+0.9°C)
  • September: +2.0°F (+1.1°C)
  • October: +1.7°F (+1.0°C)
  • November: +1.8°F (+1.0°C)
  • December: +2.2°F (+1.2°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.