ClimateSearch

Kaohsiung, Takao

Taiwan · 2.7M people · 11 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 high74°F (23°C)76°F (24°C)80°F (27°C)84°F (29°C)87°F (31°C)89°F (32°C)90°F (32°C)89°F (32°C)88°F (31°C)85°F (30°C)82°F (28°C)76°F (24°C)
Average low60°F (16°C)62°F (17°C)66°F (19°C)72°F (22°C)76°F (24°C)78°F (26°C)79°F (26°C)78°F (26°C)77°F (25°C)74°F (23°C)69°F (21°C)63°F (17°C)
Dew point57°F (14°C)59°F (15°C)63°F (17°C)68°F (20°C)73°F (23°C)76°F (24°C)76°F (24°C)76°F (25°C)74°F (24°C)71°F (22°C)67°F (19°C)60°F (16°C)
Rainfall0.7 in (18 mm)0.8 in (20 mm)1.5 in (39 mm)3 in (77 mm)8.1 in (206 mm)15.7 in (399 mm)17.9 in (454 mm)19.2 in (488 mm)8.6 in (218 mm)2.3 in (59 mm)0.8 in (19 mm)0.6 in (15 mm)
Rainy days33351114141610412
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)
Sunshine190 h178 h210 h205 h172 h143 h174 h152 h187 h205 h183 h179 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

+1.6°F (+0.9°C)

Models range from +1.4°F (+0.8°C) to +2.0°F (+1.1°C)

Days above 90°F (32°C) a year

10 → 26

About 2.8× as many

Warming by month
  • January: +1.8°F (+1.0°C)
  • February: +2.0°F (+1.1°C)
  • March: +1.7°F (+0.9°C)
  • April: +2.0°F (+1.1°C)
  • May: +1.7°F (+0.9°C)
  • June: +1.9°F (+1.1°C)
  • July: +1.7°F (+0.9°C)
  • August: +1.3°F (+0.7°C)
  • September: +1.4°F (+0.8°C)
  • October: +1.6°F (+0.9°C)
  • November: +1.5°F (+0.9°C)
  • December: +1.6°F (+0.9°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.