Welcome to Journal of University of Chinese Academy of Sciences,Today is

A Diagnosis of Moist Potential Vorticity Anomaly During Meiyu Period in 2003

  • DENG Guo ,
  • ZHOU Yu-Shu ,
  • CUI Xiao-Peng
Expand
  • 1. National Meteorological Center, Beijing 100081, China;
    2. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

Received date: 2004-09-09

  Revised date: 2004-12-16

  Online published: 2005-11-15

Abstract

By analyzing the precipitation and largescale circumfluence during the period of Meiyu in 2003,the moist potential vorticity (MPV),including the mass forcing,is used to suggest that the intensive rainfall in torrential rain system can cause anomaly of the MPV.The data diagnoses manifest that the anomaly of the MPV and the precipitation have better accordance during the period of heavyMeiyu over Changjiang river basin and Huanghe river basin in 2003.We can forecast the possible distribution and movement direction of the torrential rain system according to the impermeability of the MPV.The anomaly induced by both heat and mass forcings in the torrential rain system will be a good dynamical tracer for tracking the torrential rain region.

Cite this article

DENG Guo , ZHOU Yu-Shu , CUI Xiao-Peng . A Diagnosis of Moist Potential Vorticity Anomaly During Meiyu Period in 2003[J]. Journal of University of Chinese Academy of Sciences, 2005 , 22(6) : 712 -718 . DOI: 10.7523/j.issn.2095-6134.2005.6.009

References

[1] Ertel H.Ein Neuer gydrodynamischer Wirbelsatz.Met.Z.,1942,59:277~281.

[2] Fritsch JM,Murphy JD,Kain J S.Warm core vortex amplification over land.J.Atmos.Sci.,1994,51:1780~1807.

[3] Fritsch JM,Maddox RA.Convectively drive mesoscale weather system aloft.Part I:Observations.J.Appl.Meteorol.,1981,20:9~19.

[4] Davis CA,Weisman ML.Balanced dynamics of mesoscale vortices in simulated convective systems.J.Atmos.Sci.,1994,51:2005~2030.

[5] Skamarock WC,Weisman ML,Klemp JB.Three-dimensional evolution of simulatede long-lived squall lines.J.Atmos.Sci.,1994,51:2563~2584.

[6] Gray MEB,Shutts GJ,Craig GC.The role of mass transfer in describing the dynamics of mesoscale convective system.Quart.J.Roy.Meteor.Soc.,1998,124:1183~1207.

[7] Raymond DJ,Jiang H.A theory for long-lived mesoscale convective systems.J.Atmos.Sci.,1990,47:3067~3077.

[8] Gray MEB.An investigation into convectively generated potential-vorticity anomalies using a mass-forcing model.Quart.J.Roy.Meteor.Soc.,1999,125:1589~1605.

[9] Shutts GJ,Gray MEB.A numerical modelling study of the geostrophic adjustment process following deep convection.Quart.J.Roy.Meteor.Soc.,1994,120:1145~1178.

[10] Gao ST,Lei T,Zhou YS.Moist potential vorticity anomaly with heat and mass forcings in torrential rain systems.Chin.Phys.Lett.,2002,19(6):878~880.

[11] Gao ST,Lei T,Zhou YS,et al.Diagnostic analysis of moist potential vorticity anomaly in torrential rain systems.J.Appli.Meteoro.,2002,13:662~670 (in Chinese with English abstract).

[12] Gao ST,Zhou YS,Cui XP.Impacts of Cloud2Induced Mass Forcing on the Development of Moist Potential Vorticity Anomaly During Torrential Rains.Advanced in Atmospheric Sciences,2004,21:923~927.

[13] Gao ST,Wang XR,Zhou YS.Generation of generalized moist potential vorticity in a frictionless and moist adiabatic flow.Geophys.Res.Lett.,2004,31,L12113,doi:10.1029/2003GL019152.

[14] Zhou YS,Gao ST,Shen SP.A Diagnostic study of the structural and dynamical features of the Meiyu front system,J.Met.Soc.Japan,2004,81:1565~1576.

Options
Outlines

/