Tao Li, Li Guoping. Application of vertical component of convective vorticity vector to the diagnosis of a rainstorm brought by southwest vortex. J Appl Meteor Sci, 2012, 23(6): 702-709.
Citation: Tao Li, Li Guoping. Application of vertical component of convective vorticity vector to the diagnosis of a rainstorm brought by southwest vortex. J Appl Meteor Sci, 2012, 23(6): 702-709.

Application of Vertical Component of Convective Vorticity Vector to the Diagnosis of a Rainstorm Brought by Southwest Vortex

  • Received Date: 2011-12-26
  • Rev Recd Date: 2012-10-18
  • Publish Date: 2012-12-31
  • Convective vorticity vector (CVV) is employed to analyze the rainstorm caused by the shallow system of southwest vortex during 16—18 July 2010, using convective vorticity vector vertical component (Cz). The relationship between every component of the CVV and the 6-hour accumulated precipitation is investigated, particularly the meaning of vertical component in rainstorms caused by southwest vortex. It shows that the vertical component of CVV is a good indicator of the rainstorm caused by southwest vortex. The occurring time of strong precipitation and the peak value of vertical component of CVV are consistent. If [Cz] reaches an extreme value, the precipitation will change significantly, probably leading to heavy rain phenomenon.Thus the peak time of [Cz] can be an indicator of the heavy rain forecast. When the rainstorm begins, the precipitation region shows consistently positive values of Cz, with the heavy rain to strengthen. When the positive values of Cz expand larger, the contours become intensive, and the gradient increases. The scope of positive values of Cz and the rain belt are largely the same. In the distribution of lower troposphere 850 hPa level, the rainstorm area locates near the center of the positive values of Cz and tend to the larger gradient of Cz. The main cause is the positive vorticity advection in front of the westerly trough, so that the vorticity in southern Sichuan and eastern Sichuan enhance, and the wet isentropic surface becomes steeply. The rising movement and the water vapor deliver strengthens, which is beneficial to the formation of heavy rain. Along the vertical distribution of Cz in the storm center, the storm intensity increases significantly when vertical components from lower to higher troposphere show consistent positive values. This rainstorm case confirms that the convective vorticity vector can be used for analyzing the shallow meso-scale system like southwest vortex. However, there are very limited cases, so further validation and improvements are needed.
  • Fig. 1  24-hour accumulated precipitation during 16—17 July in 2010

    Fig. 2  500 hPa height field (solid line, unit:dagpm) and temperature field (dashed line, unit:℃)

    (a)0200 BT 16 July 2010, (b)0200 BT 17 July 2010

    Fig. 3  700 hPa height field (solid line, unit:dagpm) and wind field (vector)

    (a)2000 BT 16 July 2010, (b)0800 BT 17 July 2010

    Fig. 4  The nine-point smoothing curve of the regional average of vertical integration of CVV components in July 2010

    Fig. 5  The distribution of the vertical component Cz at 850 hPa during 16—17 July 2010 (unit: 10-10 m2·s-1·K·kg-1)

    Fig. 6  The distribution of the cross section of vertical component Cz along 30°N during 16—17 July 2010(unit:10-10 m2·s-1·K·kg-1)

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    • Received : 2011-12-26
    • Accepted : 2012-10-18
    • Published : 2012-12-31

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