A first evaluation of wave-ice interactions on the global mass balance
Sea ice frequently forms in wavy waters. Wave motion packs forming ice crystals into small floes, while the ice attenuates the waves as the ice floes increase in diameter and thickness. Swell has been reported up to a few hundred kilometres inside the ice pack. Because of ocean waves, young ice floe...
Main Authors: | , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2014
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/143575 |