ClimateSearch

Shulin, Taipei

Taiwan · 180k people · 20 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 high65°F (19°C)67°F (19°C)70°F (21°C)77°F (25°C)83°F (28°C)87°F (31°C)90°F (32°C)89°F (32°C)86°F (30°C)80°F (27°C)75°F (24°C)68°F (20°C)
Average low55°F (13°C)56°F (13°C)59°F (15°C)65°F (18°C)71°F (22°C)75°F (24°C)78°F (25°C)77°F (25°C)75°F (24°C)70°F (21°C)65°F (18°C)58°F (15°C)
Dew point53°F (12°C)54°F (12°C)58°F (14°C)64°F (18°C)70°F (21°C)74°F (24°C)76°F (24°C)76°F (24°C)73°F (23°C)67°F (20°C)63°F (17°C)56°F (13°C)
Rainfall5 in (126 mm)6.2 in (157 mm)8.3 in (210 mm)7.3 in (187 mm)9 in (230 mm)10.9 in (277 mm)10.8 in (275 mm)12.6 in (321 mm)12 in (304 mm)8.2 in (207 mm)5.6 in (142 mm)5.5 in (140 mm)
Rainy days141213131414111212111113
Snowfall0 in (0.1 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)
Sunshine74 h76 h109 h125 h137 h130 h203 h189 h172 h132 h98 h76 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

+2.0°F (+1.1°C)

Models range from +1.8°F (+1.0°C) to +2.2°F (+1.2°C)

Days above 90°F (32°C) a year

15 → 44

About 3.0× as many

Warming by month
  • January: +1.7°F (+1.0°C)
  • February: +1.6°F (+0.9°C)
  • March: +1.5°F (+0.8°C)
  • April: +2.1°F (+1.2°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.3°F (+1.3°C)
  • July: +1.9°F (+1.0°C)
  • August: +1.7°F (+0.9°C)
  • September: +2.1°F (+1.2°C)
  • October: +2.0°F (+1.1°C)
  • November: +1.9°F (+1.0°C)
  • December: +2.1°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.