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http://journals.ametsoc.org/doi/abs/10.1175/2010MWR3359.1

http://journals.ametsoc.org/doi/abs/10.1175/2010MWR3359.1 Bryan, George H., Matthew D. Parker, 2010: Observations of a Squall Line and Its Near Environment Using High-Frequency Rawinsonde Launches during VORTEX2. Mon. Wea . Rev. , 138 , 4076–4097. doi : 10.1175/2010MWR3359.1 .

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http://journals.ametsoc.org/doi/abs/10.1175/2010MWR3359.1

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  1. http://journals.ametsoc.org/doi/abs/10.1175/2010MWR3359.1 Bryan, George H., Matthew D. Parker, 2010: Observations of a Squall Line and Its Near Environment Using High-Frequency Rawinsonde Launches during VORTEX2. Mon. Wea. Rev., 138, 4076–4097. doi: 10.1175/2010MWR3359.1

  2. (negative of) density anomaly cap gets weaker with time as storm approaches time

  3. cap gets weaker with time as storm approaches time

  4. time but surface parcels are more dense too, so CIN of a surface parcel misses the story about uncapping of PBL leading to convection s3, s4 CIN of surface parcel

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