Surface Characteristics of Observed Cold Pools

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The Formation of Wider and Deeper Clouds as a Result of Cold-Pool Dynamics (2014, background): “For comparison these values are in the lower range of values observed for mesoscale convective systems over land [see Engerer et al. (2008), their Fig.”
Direct Assimilation of Radar Reflectivity without Tangent Linear and Adjoint of the Nonlinear Observation Operator in the GSI-Based EnVar System: Methodology and Experiment with the 8 May 2003 Oklahoma City Tornadic Supercell (2017, background): “16b), which prevents the low-level circulation from constructively interacting with the midlevel mesocyclones (Engerer et al. 2008; Zheng and Chen 2014); while method mixing ratio has the weakest cold pool, which is not able to enhance the midlevel mesocyclone due to the small temperature gradients…”