Abstract
During the passage of Typhoon Hinnamnor from September 5 to 6, 2022, typhoon-generated swell waves were discovered to arrive at the point of observation 20 hours before the typhoon itself entered the Sea of Japan. During the analysis of data obtained by laser instrument measuring fluid pressure variations, it was possible to determine the area of formation of the main group of swell waves generated by a passing typhoon, and to localize the area of generation of “forerunner” waves, as well as to describe the mechanisms of their formation and propagation.
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