ClimateSearch

Xizhi, Taipei

Taiwan · 205k 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 high65°F (18°C)66°F (19°C)70°F (21°C)75°F (24°C)80°F (27°C)85°F (29°C)87°F (31°C)87°F (30°C)83°F (28°C)78°F (25°C)73°F (23°C)67°F (20°C)
Average low58°F (15°C)59°F (15°C)62°F (17°C)67°F (20°C)73°F (23°C)77°F (25°C)80°F (27°C)80°F (26°C)77°F (25°C)73°F (23°C)68°F (20°C)62°F (16°C)
Dew point55°F (13°C)56°F (13°C)60°F (15°C)66°F (19°C)72°F (22°C)76°F (25°C)78°F (26°C)78°F (25°C)74°F (24°C)68°F (20°C)64°F (18°C)57°F (14°C)
Rainfall6.6 in (168 mm)6 in (153 mm)5.4 in (138 mm)5.2 in (132 mm)7.6 in (192 mm)7.4 in (188 mm)6 in (154 mm)9.1 in (231 mm)10.1 in (257 mm)11.7 in (297 mm)9.9 in (252 mm)7.8 in (199 mm)
Rainy days201717161817151818191919
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)
Sunshine145 h147 h211 h244 h272 h289 h351 h321 h288 h239 h181 h148 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

+1.9°F (+1.0°C)

Models range from +1.8°F (+1.0°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

8 24

About 3.2× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +1.7°F (+0.9°C)
  • March: +1.5°F (+0.8°C)
  • April: +2.1°F (+1.2°C)
  • May: +1.8°F (+1.0°C)
  • June: +2.2°F (+1.2°C)
  • July: +1.7°F (+1.0°C)
  • August: +1.7°F (+1.0°C)
  • September: +2.1°F (+1.2°C)
  • October: +1.9°F (+1.1°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.