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 high73°F (23°C)74°F (24°C)79°F (26°C)83°F (28°C)85°F (30°C)86°F (30°C)87°F (31°C)86°F (30°C)86°F (30°C)83°F (28°C)80°F (26°C)74°F (24°C)
Average low59°F (15°C)61°F (16°C)65°F (19°C)71°F (22°C)75°F (24°C)77°F (25°C)78°F (25°C)77°F (25°C)76°F (24°C)73°F (23°C)69°F (20°C)62°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)
Rainfall1.4 in (37 mm)1.2 in (31 mm)1.6 in (41 mm)3.8 in (96 mm)10 in (253 mm)14.4 in (366 mm)11.7 in (298 mm)15.4 in (392 mm)7.9 in (200 mm)2.8 in (72 mm)1.9 in (47 mm)1.5 in (38 mm)
Rainy days6681118212222181175
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)
Sunshine272 h263 h314 h311 h300 h282 h310 h281 h301 h310 h273 h264 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.