tájfunok

Tájfunok are intense tropical cyclones that form over the western Pacific Ocean. They are characterized by a low-pressure center, strong winds, and heavy rainfall, often causing widespread destruction. The term "tájfun" is specifically used for these storms in the Northwest Pacific Basin.

The formation of a tájfun begins with warm ocean waters, typically above 26.5 degrees Celsius, providing the necessary energy. This warm, moist air rises and condenses, creating thunderstorms. As more air is drawn into the system, it begins to rotate due to the Earth's rotation (the Coriolis effect). If conditions remain favorable, the storm can intensify, developing a distinct eye at its center, a region of calm weather.

Tájfunok can reach wind speeds exceeding 250 kilometers per hour, making them among the most powerful weather phenomena on Earth. Their impact extends beyond strong winds, as they also bring torrential rain, leading to significant flooding and landslides. Storm surges, a rise in sea level caused by the storm's winds and low pressure, can inundate coastal areas.

The deadliest and costliest tájfun in recorded history was the 1975 Typhoon Nina, which caused catastrophic flooding in China. Due to their destructive potential, tájfunok are closely monitored by meteorological agencies, and timely warnings are crucial for evacuations and disaster preparedness in affected regions, particularly in East and Southeast Asia.