ClimateSearch

Nantou, Taiwan

Taiwan · 106k people · 205 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 high68°F (20°C)69°F (20°C)73°F (23°C)78°F (26°C)83°F (28°C)86°F (30°C)88°F (31°C)87°F (30°C)85°F (30°C)81°F (27°C)77°F (25°C)71°F (22°C)
Average low55°F (13°C)56°F (14°C)61°F (16°C)67°F (19°C)72°F (22°C)75°F (24°C)76°F (25°C)75°F (24°C)74°F (24°C)69°F (21°C)64°F (18°C)58°F (14°C)
Dew point52°F (11°C)54°F (12°C)58°F (15°C)64°F (18°C)68°F (20°C)71°F (22°C)72°F (22°C)72°F (22°C)70°F (21°C)66°F (19°C)61°F (16°C)55°F (13°C)
Rainfall1.4 in (36 mm)2.4 in (60 mm)4.7 in (119 mm)5.5 in (141 mm)9.1 in (231 mm)13.9 in (353 mm)18.2 in (463 mm)16.1 in (409 mm)6.9 in (176 mm)1.3 in (34 mm)0.6 in (16 mm)1.3 in (33 mm)
Rainy days681091215181911225
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)
Sunshine204 h182 h213 h198 h178 h146 h174 h153 h183 h217 h205 h200 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

+1.7°F (+1.0°C)

Models range from +1.5°F (+0.9°C) to +1.9°F (+1.1°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.2°C)
  • February: +2.3°F (+1.3°C)
  • March: +1.9°F (+1.1°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +1.6°F (+0.9°C)
  • August: +1.4°F (+0.8°C)
  • September: +1.1°F (+0.6°C)
  • October: +1.4°F (+0.8°C)
  • November: +2.2°F (+1.2°C)
  • December: +2.3°F (+1.3°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.