Abstract:
Differential reflectivity (
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
) arc is known as an arc-shaped region of high differential reflectivity along the inflow edge of the forward flank, while a down shear elongated
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
maximum near the echo centerline of the storm is known as
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot. The
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc and the clear horizontal separation between the areas of
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc and
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot have been confirmed to be the signatures of hydrometeor size sorting within their forward flank regions in supercell storms. Recent studies have indicated that
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc and
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc-
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot separation signatures insupercell storms may be related to environmental storm-relative helicity and low-level shear. Based on the conception model and machine learning, the recognition algorithm for
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot and
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc is designed, and the separation and angle of
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc and
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot are then calculated. The recognition effect and quantitative calculation are examined using S band polarimetric radar and auto weather station observations of four supercell storms occurred in East China. The results show that the recognition method introduced in this study can identity
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc and
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot correctly, the variation of
Z_\mathrmD\mathrmR ![](CN20220007_M26.jpg)
arc-
K_\mathrmD\mathrmP ![](CN20220007_M27.jpg)
foot centroid distance and separation angle can indicate the occurrence of extreme gust.