tájfun

Tájfun is a term used in East Asia and Southeast Asia for a mature tropical cyclone that develops in the northwestern Pacific Ocean. This region is characterized by warm ocean waters and atmospheric conditions conducive to the formation and intensification of such storms. A tájfun is essentially the same phenomenon as a hurricane in the Atlantic or a cyclone in the Indian Ocean, differing only in its geographical location and the specific name given to it.

These powerful rotating storm systems form over tropical or subtropical waters and are fueled by heat and moisture from the ocean. They are characterized by a low-pressure center, strong winds spiraling inward, and heavy rainfall. The intensity of a tájfun is typically measured using scales like the Saffir-Simpson Hurricane Wind Scale, adapted for the region.

Tájfun activity is most common during the summer and early autumn months in the Northern Hemisphere, when sea surface temperatures are at their highest. These storms can cause significant damage due to high winds, torrential rain leading to flooding, and storm surges that inundate coastal areas. Their paths can be unpredictable, making monitoring and preparedness crucial for populations in affected regions. Nations along the western Pacific rim, including the Philippines, Japan, China, and Vietnam, are particularly vulnerable to tájfun impacts.