摘要
Based on modifications of the observed background parabolic current in upper layer of the northeastern South China Sea （SCS）, the effects of eight kinds of background currents on the characteristics and energy conversion of internal solitary waves （ISWs） are investigated by an Internal Gravity Wave （IGW） model. It is found that, although the background current has little effect on the number of the generated ISWs, it reduces the resulted phase speed of ISW. When the background parabolic current appears with its lower boundary near or above the main thermocline, the ISW amplitude and the depth of the isopycnal undergoing maximum displacement increase; when the background parabolic current curvature is reduced, the ISW amplitude and the ratio of baroclinic to barotropic energy reduce, whilst the phase speed of ISW, the baroclinic energy, and the ratio of baroclinic kinetic energy （KE） to available potential energy （APE） increase; when the lower boundary of background parabolic current extends down to the seabed and the background current curvature is reduced, the ISW amplitude and phase speed decrease, whilst the barotropic kinetic energy, the baroclinic energy and the ratio of KE to APE increase. At a whole depth, when the lower background current curvature is reduced and the upper current curvature is increased, the ISW amplitude, and phase speed, the ratio of baroclinic to barotropic energy, the baroclinic energy, and the ratio of KE to APE all increase.
Based on modifications of the observed background parabolic current in upper layer of the northeastern South China Sea （SCS）, the effects of eight kinds of background currents on the characteristics and energy conversion of internal solitary waves （ISWs） are investigated by an Internal Gravity Wave （IGW） model. It is found that, although the background current has little effect on the number of the generated ISWs, it reduces the resulted phase speed of ISW. When the background parabolic current appears with its lower boundary near or above the main thermocline, the ISW amplitude and the depth of the isopycnal undergoing maximum displacement increase; when the background parabolic current curvature is reduced, the ISW amplitude and the ratio of baroclinic to barotropic energy reduce, whilst the phase speed of ISW, the baroclinic energy, and the ratio of baroclinic kinetic energy （KE） to available potential energy （APE） increase; when the lower boundary of background parabolic current extends down to the seabed and the background current curvature is reduced, the ISW amplitude and phase speed decrease, whilst the barotropic kinetic energy, the baroclinic energy and the ratio of KE to APE increase. At a whole depth, when the lower background current curvature is reduced and the upper current curvature is increased, the ISW amplitude, and phase speed, the ratio of baroclinic to barotropic energy, the baroclinic energy, and the ratio of KE to APE all increase.
基金
The National Basic Research Program(973 Program)under contract Nos 2013CB956101 and 2011CB013701
the Strategic Priority Research Program of the Chinese Academy of Sciences under contract No.XDA11020201
the National Natural Science Foundation of China under contract Nos 41406019,41406025,41430964 and 41025019
the CAS/SAFEA International Partnership Program for Creative Research Teams under contract No.20140491532
