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大气定常波传播的运动学特征的时空变化 被引量:1

SPAC1AL AND TEMPERAL VARIATION OF THE KINEMATIC CHARACTERISTICS FOR THE PROPAGATION OF ATMOSPHERIC STATIONARY WAVES
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摘要 利用时间平均全球大气环流资料,本文计算了纬向平均位涡的南北梯度的时空分布,以及波动水平传播的临界波数n_s,和垂直传播的临界波数K_c的时空分布。由此研究全球大气定常波传播的运动学特征及其年变化。 Time-mean global general circulation data are employed to analyse the temperal and spatial variation of the meridional gradient of zonal mean potential vorticity, the critical wave number nc for horizontal wave-propagation, and the critical wave number Kc for vertical wave-propagation. Thereby the kinematic characteristics for the propagation of atmospheric stationary waves an.d their annual variations are studied. Results show that in the troposphere nc and Kc usually decrease with the increase of either latitude or altitude. Synoptic and near-resonant Rossby waves could be trapped during their upward and meridional propagations. These characteristics possess prominent annual variations, especially in the Northern Hemisphere. It is found that the spatial and temperal variations of these kinematic characteristics are in good agreement with those of the atmospheric wave patterns.
出处 《气象学报》 CSCD 北大核心 1990年第1期36-45,共10页 Acta Meteorologica Sinica
基金 国家自然科学基金~~
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参考文献2

  • 1吴国雄,大气科学,1988年,94页
  • 2吴国雄,全球大气环流时间平均统计图集,1987年

同被引文献37

  • 1陆维松.球面定常行星波的几种传播路径[J].气象学报,1989,47(2):221-226. 被引量:7
  • 2宋燕,缪锦海.经圈环流对定常波传播的影响[J].气象学报,1994,52(4):424-432. 被引量:2
  • 3吕克利,朱永春.大地形对Rossby波波射线的影响[J].气象学报,1994,52(4):405-413. 被引量:5
  • 4季劲钧.大气经圈环流对波动和能量传输的影响[J].大气科学,1990,14(4):413-421. 被引量:4
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  • 6Rossby C G.Relations between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semipermanent centers of action. J.Mar. Res.,1939,3:38-55.
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  • 8Charney J G,Drazin P G.Propagation of planetary-scale disturbances from the lower into the upper atmosphere.J.Geophys.Res.,1961,66(1):83-109.
  • 9Eliassen A,Plam E.On the transfer of energy in stationary mountain waves.Geofysiske Publikasjoner,1961,22(3):1-23.
  • 10Matsuno T.Vertical propagation of stationary planetary waves in the winter Northern Hemisphere.J.Atmos.Sci.,1970,27(6):871-883.

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