Refractive Index of the Ionosphere | Derivation Simplified | Sky Wave / Ionospheric Propagation

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  • เผยแพร่เมื่อ 3 ธ.ค. 2024

ความคิดเห็น • 13

  • @mananbahl4842
    @mananbahl4842 2 ปีที่แล้ว +6

    Legend made complex topic so eeaasssyyyyyy no one on yt has done it so welll
    God bless you

  • @lagansharma8181
    @lagansharma8181 ปีที่แล้ว +3

    Thank you so much sir❤
    Really appreciable ur efforts
    All other videos are very boring nd time consuming
    Ur videos very interesting nd easy to learn and watch thank you sir☺

  • @Kendergil
    @Kendergil 3 ปีที่แล้ว +2

    You are so enthusiastic. That’s very encouraging. 🙂

  • @alisterrozario3997
    @alisterrozario3997 3 ปีที่แล้ว +4

    Good class very interisting and good method

    • @BackbenchEngineer
      @BackbenchEngineer  3 ปีที่แล้ว

      Hey Alister!! Thanks buddy!! Really happy to hear that!! More such videos are in the making so do join our community by hitting that subscribe button so that you will be updated as soon as the videos are out!! Do share it with your friends as well!!

  • @abhishekchakraborty9988
    @abhishekchakraborty9988 2 ปีที่แล้ว +3

    Explanation is nice just one suggestion I would like to give is try to speak normally otherwise people will not take your videos seriously....This might be the reason for such a low subscriber count

  • @ammukutty9264
    @ammukutty9264 2 ปีที่แล้ว +1

    Very informative thanku sir

  • @tsehayenegash8394
    @tsehayenegash8394 3 ปีที่แล้ว +1

    How can I calculate temperature,prssure and water vapor from refractivity in the neutral atmosphere

    • @BackbenchEngineer
      @BackbenchEngineer  3 ปีที่แล้ว +4

      Hello Tsehaye Negash.
      Greetings from The Backbench Engineering Community.
      Briefly answering your query here.
      We know that refractivity is height dependent and different mathematical models exist that approximately represent the refractivity profile.
      For average atmosphere , accepted standard value for vertical gradient is give as deltaN = 39 per km.
      The standard radio atmosphere is based on linear model given as N = Ns + DeltaN ( H - Hs ).
      But it is seen that further other models also exist for the same.
      In further models, the relation between dry Height and surface temperature was expressed as Hd = 40.082 + 0.14898 ts.
      Please mail us at backbench4006@gmail.com for full clarification and documents related to your query.
      The query is very much appreciated even though it is not related to the syllabus discussed here. Looking forward to having a discussion with you regarding this over mail.
      Thanks & Regards
      The Backbench Engineering Community

  • @vigneshs1620
    @vigneshs1620 3 ปีที่แล้ว +1

    👍

  • @fathimanazeer3101
    @fathimanazeer3101 3 ปีที่แล้ว +3

    👍🙂