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 high64°F (18°C)65°F (18°C)69°F (21°C)76°F (24°C)81°F (27°C)85°F (30°C)88°F (31°C)87°F (31°C)84°F (29°C)78°F (25°C)73°F (23°C)66°F (19°C)
Average low55°F (13°C)55°F (13°C)58°F (14°C)64°F (18°C)70°F (21°C)75°F (24°C)77°F (25°C)77°F (25°C)74°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)
Rainfall3.6 in (91 mm)3.9 in (99 mm)4.4 in (111 mm)5.3 in (134 mm)8 in (204 mm)10.1 in (257 mm)8.6 in (218 mm)11.4 in (290 mm)9.7 in (247 mm)8.1 in (206 mm)5.2 in (131 mm)4.1 in (105 mm)
Rainy days141214161921192117161515
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)
Sunshine148 h151 h207 h233 h260 h271 h339 h307 h276 h229 h181 h151 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.