Kaohsiung Hit by Typhoon-Like Winds; Meteorological Station Explains Cause

Kaohsiung experienced unusually strong winds on July 13 and 14, leading residents to compare the conditions to a typhoon passing through the region. The Kaohsiung Meteorological Station has explained the phenomenon, citing specific atmospheric conditions.

The intense gusts were primarily caused by the combined influence of a tropical disturbance located southwest of Taiwan in the South China Sea and the Pacific high-pressure system to the east. This interaction increased the pressure gradient near Taiwan, significantly strengthening the southerly winds. Additionally, the topography of the Central Mountain Range likely amplified these winds further in coastal and open areas of Kaohsiung.

According to the Meteorological Station, the strongest winds were recorded at the Nanliao station in Mituo District on July 13. This station registered a maximum average wind speed of level 7 and a maximum gust speed of level 9. These powerful winds were forecast to persist through July 14, keeping Kaohsiung within the range of the strong wind advisory issued by the Central Weather Administration.

Residents described the wind as relentless, prompting curiosity about its cause. The Meteorological Station's explanation provided clarity on the meteorological factors at play, assuring the public that the strong winds were a result of predictable atmospheric dynamics rather than an actual typhoon.