In this paper, both direct method and its application to wave-wave striking interaction are introduced by illustrating Schrodinger equation describing the amplitude evalution of some mesoscale systems.
McFarline's gravity drag theory is simply reviewed,and it is indicated that the fault of McFarline's theory is that the effect of dissipation induced by gravity wave breaking on mean flow is not fully consider...McFarline's gravity drag theory is simply reviewed,and it is indicated that the fault of McFarline's theory is that the effect of dissipation induced by gravity wave breaking on mean flow is not fully considered.Based on McFarline's theory,in this paper,the effect mentioned above is well considered.A new dissipation coefficient D is calculated,and a relatively complete parameterized scheme of the influence of gravity wave breaking on meanflow is put forward here. This is a better parameterized scheme than McFarline's if it is used in GCM.展开更多
文摘In this paper, both direct method and its application to wave-wave striking interaction are introduced by illustrating Schrodinger equation describing the amplitude evalution of some mesoscale systems.
基金This work was supported by the National Natural Science Foundation of China under Grant No.49675257
文摘McFarline's gravity drag theory is simply reviewed,and it is indicated that the fault of McFarline's theory is that the effect of dissipation induced by gravity wave breaking on mean flow is not fully considered.Based on McFarline's theory,in this paper,the effect mentioned above is well considered.A new dissipation coefficient D is calculated,and a relatively complete parameterized scheme of the influence of gravity wave breaking on meanflow is put forward here. This is a better parameterized scheme than McFarline's if it is used in GCM.
