巢纪平. 2000: 论热带纬圈半地转运动的建立. 气象学报, (2): 129-136. DOI: 10.11676/qxxb2000.014
引用本文: 巢纪平. 2000: 论热带纬圈半地转运动的建立. 气象学报, (2): 129-136. DOI: 10.11676/qxxb2000.014
Chao Jiping. 2000: ON THE FOUNDATION OF ZONAL SEMI-GEOSTROPHIC MOTION IN TROPICS. Acta Meteorologica Sinica, (2): 129-136. DOI: 10.11676/qxxb2000.014
Citation: Chao Jiping. 2000: ON THE FOUNDATION OF ZONAL SEMI-GEOSTROPHIC MOTION IN TROPICS. Acta Meteorologica Sinica, (2): 129-136. DOI: 10.11676/qxxb2000.014

论热带纬圈半地转运动的建立

ON THE FOUNDATION OF ZONAL SEMI-GEOSTROPHIC MOTION IN TROPICS

  • 摘要: 文中在赤道β平面上,在滤掉低频Rossby波的情况下,研究了纬圈半地转运动的建立。指出,只有当运动的纬圈尺度很大时,非地转风分量才能随着重力惯性波的频散而消失,从而建立起纬圈半地转平衡。应用位势涡度不变式,给出了纬圈半地转适应后物理场的解。同时指出,Kelvin波(对赤道对称情况)和混合波的Rossby波波段(对赤道反对称情况)将不参与适应运动,它们属于发展运动中的角色。

     

    Abstract: On the equat orial β-plane the foundation of zonal semi-geostrophic motion is investigated.It is indicated that, only under the condition that the zonal scale is large, the non-geostrophic wind is dispersed with the disper sion of gravity -inertia wave, and the time conservation of the vorticity is established.The Kelvin wave and Rossby short wave in mixed wave will participate the evolution stage not participate the adjustment stage of motion.

     

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