On 1 January 1995 at 15 UTC, the most famous freak wave to be detected by a measuring instrument was recorded by a downward-looking laser at the North Sea Draupner gas platform. The wave was 25.6 m high, with an 18.5 m crest height (Box A). The significant wave height in the area northwest). Over the next 12 hours (Figure 1b-c), the polar is estimated to have been almost 12 m. The measurement confirmed the existence of giant rogue waves, which had previously been reported anecdotally by sailors. It prompted a number of studies which aimed to determine the meteorological and wave situation at the time and to provide a physical explanation of the event.
What conditions led to the Draupner freak wave?
Luigi Cavaleri;Luciana Bertotti;Francesco Barbariol;Alvise Benetazzo;
2016
Abstract
On 1 January 1995 at 15 UTC, the most famous freak wave to be detected by a measuring instrument was recorded by a downward-looking laser at the North Sea Draupner gas platform. The wave was 25.6 m high, with an 18.5 m crest height (Box A). The significant wave height in the area northwest). Over the next 12 hours (Figure 1b-c), the polar is estimated to have been almost 12 m. The measurement confirmed the existence of giant rogue waves, which had previously been reported anecdotally by sailors. It prompted a number of studies which aimed to determine the meteorological and wave situation at the time and to provide a physical explanation of the event.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
