Gravity Waves and Aperiodic Modes in Kinematically Complex Flows

 
Elene Chkhartishvili
Free University of Tbilisi
Advisor: Andria Rogava
 
The Dynamics of
Gravity Waves and
Aperiodic Modes in
Kinematically
Complex Flows
 
01
 
The
Phenomenon
 
Table of Contents
 
02
 
Main
Formalism
 
03
 
Calculations and
Findings
 
04
 
Future
Perspectives
 
The Phenomenon
 
01
 
Internal and surface gravity waves,
simulation
What Are Gravity Waves ?
Internal gravity waves occur in
density stratified fluids in the
presence of a gravitational
field. They arise as
gravitational restoring forces
act on vertically displaced
fluid.
 
Gravity Waves in Nature
 
Main Formalism
 
02
 
Main theory and formalism
 
Main Theory
 
Background Velocity Field
 
Shear Matrix
 
Spatially Inhomogenous Operator
 
Linearization of The Velocity Field
 
Eliminating The Spatial Dependency
 
Calculations and Findings
 
03
 
Main equations and the incompressible case
 
Main Equations
 
Working Shear Matrix
 
Equations For T
he
Wavenumber Vector
Components
 
Equations for the Incompressible Case
 
Equations for the Velocity
Vector Components
 
Other Important Equations
 
Findings and Derivations
 
Eliminating the First Order Differential Term
 
Eliminating the First Order Differential Term
 
Future Perspectives
 
04
 
Future Perspectives
 
Numerical
Computations
 
Helioseismology
 
Natural
Phenomena
 
Thank you !!
 
Do you have any questions?
 
Elene Chkhartishvili
Free University of Tbilisi
Advisor: Andria Rogava
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Delve into the dynamics of gravity waves and aperiodic modes in kinematically complex flows in this detailed study by Elene Chkhartishvili from Free University of Tbilisi. The research covers topics like internal gravity waves, main formalism, linearization of the velocity field, main equations, and insights into the incompressible case. Discover the phenomena, calculations, findings, and future perspectives related to gravity waves and their behavior in nature.

  • Gravity Waves
  • Aperiodic Modes
  • Kinematically Complex Flows
  • Research Study
  • Fluid Dynamics

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  1. Elene Chkhartishvili Free University of Tbilisi Advisor: Andria Rogava The Dynamics of Gravity Waves and Aperiodic Modes in Kinematically Complex Flows

  2. Table of Contents 01 The Phenomenon 03 Calculations and Findings 02 Main Formalism 04 Future Perspectives

  3. Internal and surface gravity waves, simulation 01 The Phenomenon

  4. What Are Gravity Waves ? Internal gravity waves occur in density stratified fluids in the presence of a gravitational field. They arise as gravitational restoring forces act on vertically displaced fluid.

  5. Gravity Waves in Nature

  6. Main theory and formalism 02 Main Formalism

  7. Main Theory Background Velocity Field ? ?,?,? = ???,?,? ??+ ???,?,? ??+ ???,?,? ?? Shear Matrix ??,? ??,? ??,? ??,? ??,? ??,? ??,? ??,? ??,? ?11 ?21 ?31 ?12 ?22 ?32 ?13 ?23 ?33 ?

  8. Linearization of The Velocity Field ???,?,? ??(?0,?0,?0) + ????? Spatially Inhomogenous Operator ? ??+ ??(?,?,?)?? Eliminating The Spatial Dependency ? ?,?,?;? ? ? ? ,? ??? ?? = ????? ? ? ??? ?? ?0? ??? ??

  9. Main equations and the incompressible case 03 Calculations and Findings

  10. Main Equations ?? The transposed Shear Matrix ? Time-Dependent Wavenumber Vector ??? + ?? ? = 0 ? ?2 ?1 ? Working Shear Matrix ? = (1)= ??? ?2?? (1)= ?1??+ ??? ?? ?? ?? Equations For The Wavenumber Vector Components (1)= 0

  11. Equations for the Incompressible Case Equations for the Velocity Vector Components ? Dimensionless Notation of the Pressure Perturbations ? Frequency (1)= ??? ?1?? ??? ?? Other Important Equations (1)= ?2??+ ??? ??? ?? ????+ ????+ ????= 0 (1)= ??? + ??? ?? (1)?? ???? 1= ????? = ?? ?(1)= ?? ???? ???? ? = ??2 ?? ????+ ????

  12. Findings and Derivations 2 2 2 2ln ? ?2 2 2 (2) ?? 1+ ?2? ?2+2 ?1 ?2?? = ?2 ? ? 2 ?2 ?2? Eliminating the First Order Differential Term 2 1 2 ? ?2 2??2 2 ?2 ??4 2?2 ??2 2? (3? 2?2 2 3 2) = ?2 ? ? (2)+ + 2 ? ? 2; ?2= ? 2; 2= ?2+ ?1?2; ? = ?????. 2= ?? 2+ ?? 2+ ?? ? ???: ?

  13. Eliminating the First Order Differential Term (2)+ ? ? 1+ ? ? = ? ? = ? After differentiating and plugging into the initial equation: ? (2)+ 2?1+ ?? 1+ ?? + ??1+ ?2 = ? So, if we choose 2?1= ??, then the first order derivative will vanish, and we will be left with the equation: (2)+ ? + ??1 ?+?2 ? ?. = ? 2 2 ??2ln ? 2?2 In our case, ?(1) . ?= 2 ? ?2, which we can plug into the equation to finish the elimination process. From this, ? =

  14. 04 Future Perspectives

  15. Future Perspectives Numerical Computations Natural Phenomena Helioseismology

  16. Do you have any questions? Elene Chkhartishvili Free University of Tbilisi Advisor: Andria Rogava CREDITS: This presentation template was Flaticon created by Slidesgo, and includes icons by Flaticon and infographics & images by Freepik Slidesgo Freepik Thank you !!

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