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ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS

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  • On the basis of the budget equations for KR and KD, this paper presents the horizontal pattern of budget terms for two kinds of low level jets (LLJ) with and without heavy rain. The results show that the mechanisms for generating and maintaining LLJ are different, and especially, the direction of energy conversion is opposite. A positive conversion from KD to KR appears to be a necessary but not sufficient condition in the lower troposphere near the heavy rain area. The intensity and direction of energy conversion depends not only on the relative position of vorticity and divergence field, but also on the vertical profile of the jets directly.
  • [1] Buechler D E,Fuelberg H E,1986. Budget of divergent and rotational kinetic energy during two periods of intense convection. Mon.wea. Rev.,114:95-114.
    [2] Endlich R M,1967. An interative method for altering the kinetic properties of wind field. J. Appl. Met.,6:837-844.
    [3] Wang Zhongxing, 1992. The characteristics of budget for divergent and rotational component of kinetic energy in heavy rain processes. J. China University of Sci & Tech.,22:342-347 (in Chinese).
    [4] Wang Zhongxing,1993. The characteristics of conversion between kinetic energies of divergent and rotational winds during heavy rain period. Scientia Atmospherics Sinica,17:185-191 (in Chinese).

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Wang Zhongxing, Jiao Meiyan. ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS [J]. Journal of Tropical Meteorology, 1996, 2(2): 189-193.
Wang Zhongxing, Jiao Meiyan. ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS [J]. Journal of Tropical Meteorology, 1996, 2(2): 189-193.
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Manuscript History

Manuscript received: 06 June 1994
Manuscript revised: 28 November 1994
通讯作者: 陈斌, bchen63@163.com
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ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS

Abstract: On the basis of the budget equations for KR and KD, this paper presents the horizontal pattern of budget terms for two kinds of low level jets (LLJ) with and without heavy rain. The results show that the mechanisms for generating and maintaining LLJ are different, and especially, the direction of energy conversion is opposite. A positive conversion from KD to KR appears to be a necessary but not sufficient condition in the lower troposphere near the heavy rain area. The intensity and direction of energy conversion depends not only on the relative position of vorticity and divergence field, but also on the vertical profile of the jets directly.

Wang Zhongxing, Jiao Meiyan. ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS [J]. Journal of Tropical Meteorology, 1996, 2(2): 189-193.
Citation: Wang Zhongxing, Jiao Meiyan. ENERGETIC DIAGNOSIS FOR TWO KINDS OF LOW LEVEL JETS [J]. Journal of Tropical Meteorology, 1996, 2(2): 189-193.
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