Study on the Dynamic Process of the Onset of South China Sea Summer Monsoon |
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| Authors: | ZHANG Lifeng ZHANG Yongchui and ZHANG Ming |
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| Institution: | Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101;Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101;Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101 |
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| Abstract: | By using the NCEP/NCAR reanalysis data from 1958 to 1997,we first looked into the atmospheric flow conditions in the one month immediately prior to the onset of the South China Sea summer monsoon (SCSSM) each year.A monthly-averaged zonal basic flow of 40-yr composite was then calculated.The stability of Rossby wave in the basic flow was studied based on the spherical harotropic vorticity equation. Furthermore,the spectral function expansion method was adopted to define and compute the evolvement of a developing wave packet.The results indicate that there exists barotropic instability of spherical Rossby wave in the climatically-averaged flow field before the SCSSM onset.The instability is triggered by the westerly jet stream in the Southern Hemisphere,and the strongest instable perturbation lies to the south of the westerly jet stream.The peak of the developing spherical Rossby wave packet propagates from mid and high latitudes to low latitudes,though not crossing the equator,spurring the cumulus convection in the tropical zones.The eruption of the cumulus convection and its spread to monsoon regions help to speed up the adjustment of the general circulation and the SCSSM onset.It is concluded that elements that contribute to the SCSSM onset are on global scale,albeit the onset itself looks like a local phenomenon. |
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| Keywords: | SCSSM onset spherical barotropic instability tropic cumulus convection developing wave packet dynamic process |
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