Three-Dimensional Storm Structure and Low-Level Boundaries at Different Stages of Cyclic Mesocyclone Evolution in a High-Precipitation Tornadic Supercell

<div>MGAUS sounding in Minco, OK, at 0008 UTC on 30 May 2004. In (a) is the thermodynamic sounding with parameters in the upper right-hand corner. In (b) is the hodograph with the 0–3 km storm-relative helicity shaded in grey and an arrow indicating the average storm motion.</div>

Advances in Meteorology

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Figure 2

Figure 2: Three-Dimensional Storm Structure and Low-Level Boundaries at Different Stages of Cyclic Mesocyclone Evolution in a High-Precipitation Tornadic Supercell 

Figure 2 | Three-Dimensional Storm Structure and Low-Level Boundaries at Different Stages of Cyclic Mesocyclone Evolution in a High-Precipitation Tornadic Supercell 