METR2023 - Lecture 15 - Segment 3: Using Potential Vorticity to Explain Lee Cyclogenesis

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  • Опубликовано: 19 дек 2024

Комментарии • 7

  • @shawnharrison7596
    @shawnharrison7596 Год назад

    Red Flag Warnings (dry dusty air) popped up in a large area of New Mexico and then shortly after, the Cole Oklahoma tornado of April 19th 2023 happened.

  • @shawnharrison7596
    @shawnharrison7596 Год назад

    What about the electrostatic induction from dust particles from Utah, Arizona, New Mexico coming from Point A going over Point B and descending at Point C and influencing the curl factor of the vorticity potential?

  • @timmogaasbeek
    @timmogaasbeek Год назад

    thanks for this very interesting series of lectures. i'm thoroughly enjoying learning more about meteorology in the process. just one question about this segment: what column do you take to calculate delta z? is that ground level to tropopause, or can you also take a lower pressure level?

    • @davidstang2188
      @davidstang2188  Год назад +1

      I'm glad to hear that you're enjoying the material! To answer your question, the term ∆z is usually taken as the distance between the ground and the tropopause. The reason for this is because you'll see potential vorticity (PV) anomalies at the tropopause, which violates the conservation law shown in the video.

  • @himadribaguli7880
    @himadribaguli7880 2 года назад

    Good 👍

  • @rik9217
    @rik9217 4 года назад

    Thank you!

  • @Davidstang
    @Davidstang 4 года назад

    Nice mr stang