Analysis of Vorticity during Vortex Producing Snowstorm in North China in Winter
Yuanchun Zhang, Sun Jian-hua, Shenming Fu
Abstract
Yuanchun Zhang, Sun Jian-hua, Shenming Fu
Abstract
The snowstorm occurred in North China on 2~3 January 2010 was simulated using WRF model.And potential vorticity and vorticity equation were used to diagnose the developing mechanism of the vortex producing heavy snowfall process in winter.The results showed that,firstly,the weak trough in middle troposphere leaded to lower and surface systems moving from west to east.Secondly,potential vorticity from upper-level intensified development of vortex in middle-lower troposphere.Thirdly,the mean flux and stretching term of the integrated vorticity equation was the main source of vorticity,but eddy flux and like-tilt term was relatively weak.During the mature period of vortex,the vorticity decreased because of the divergence of environmental circulation to vortex area while the vortex moved faster than surrounding air,and to the contrary,vorticity increased for the convergence between environmental circulation and vortex area.During the dissipating period,the vorticity decreased since the loss of the absolute vorticity flux.On the basis of all diagnosis,the PV forcing in upper-troposphere,convergence in lower-troposphere and the vorticity produced by environmental circulation are main mechanisms of vorticity developing.
OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The snowstorm occurred in North China on 2~3 January 2010 was simulated using WRF model.And potential vorticity and vorticity equation were used to diagnose the developing mechanism of the vortex producing heavy snowfall process in winter.The results showed that,firstly,the weak trough in middle troposphere leaded to lower and surface systems moving from west to east.Secondly,potential vorticity from upper-level intensified development of vortex in middle-lower troposphere.Thirdly,the mean flux and stretching term of the integrated vorticity equation was the main source of vorticity,but eddy flux and like-tilt term was relatively weak.During the mature period of vortex,the vorticity decreased because of the divergence of environmental circulation to vortex area while the vortex moved faster than surrounding air,and to the contrary,vorticity increased for the convergence between environmental circulation and vortex area.During the dissipating period,the vorticity decreased since the loss of the absolute vorticity flux.On the basis of all diagnosis,the PV forcing in upper-troposphere,convergence in lower-troposphere and the vorticity produced by environmental circulation are main mechanisms of vorticity developing.
Key concepts: Positive vorticity advection, Vorticity, Vortex stretching, Vorticity equation, Potential vorticity, Vortex, Troposphere, Atmospheric sciences