The decaying typhoon, tropical storm Prapiroon, is no threat to land, safely positioned 325 nautical miles south of Yokosuka, Japan, headed out to sea.
...[W]hen fluids encounter obstacles, they can form spiral eddies. The air-flow obstacle responsible for these vortices was likely Cheju (Jeju) Island. A volcanic peak on Cheju, Halla Mountain, rises to 1,950 meters (6, 398 feet) above sea level. The spiral eddies extended about 720 kilometers (450 miles) south of the island.
As the winds (clouds) reach the island, they are split by the volcano. As the flow moves around the volcano, it creates an off-centered area of low pressure in its wake, in effect a whirlpool or vortex.
As this vortex moves off, another vortex is created, alternately off-centered. This vortex again moves off repeating the process and creating these remarkable patterns in the island’s wake as long as the wind speed and direction will support it.