SIMULATION OF THE HYDROELASTIC RESPONSE OF A FLOATING ICE SHEET
Introduction In the polar region,ice sheets can be several kilometres long and subjected to the effects of ocean waves.As its thickness to length ratio is very small,an ice sheet may experience significant localised vibrations under continuous wave excitation.In such situations,the vibratory response of the large ice sheet is dominated by an elastic deformation rather than rigid body motions,which is also known as the hydroelastic response of sea ice.A review on this phenomenon has been given by Squire 1,indicating that understanding it fully will be a key challenge of polar engineering.The hydroelastic waveice interaction can induce wave reflection and transmission 2,which makes the wave field nearby very different from that in the open ocean and can lead to a considerable influence on any adjacent structures and/or passing vessels.
Fluid-Structure Interaction Hydroelasticity Sea Ice Ocean Surface Wave OpenFOAM
LUOFENG HUANG MINGHAO LI (Z)ELJKO TUKOVI(C) GILES THOMAS
University College London,UK Chalmers University of Technology,Sweden University of Zagreb,Croatia
国际会议
The 13th OpenFOAM Workshop(第13届OpenFOAM国际研讨会)
上海
英文
213-216
2018-06-24（万方平台首次上网日期，不代表论文的发表时间）