PARS Workshop on Novel Methods of Excitation of ULF/ELF/VLF to Improve Efficiency and Availability" November 3 - 6, 2002 Sponsored by Air Force Research.

Slides:



Advertisements
Similar presentations
Chapter 3 – Radio Phenomena
Advertisements

HOW DOES MY SIGNAL GET FROM HERE TO THERE? By Forest Cummings, W5LQU And Dave Russell, W2DMR.
Using a DPS as a Coherent Scatter HF Radar Lindsay Magnus Lee-Anne McKinnell Hermanus Magnetic Observatory Hermanus, South Africa.
Pitch-Angle Scattering of Relativistic Electrons at Earth’s Inner Radiation Belt with EMIC Waves Xi Shao and K. Papadopoulos Department of Astronomy University.
Efficiency in ELF/VLF Generation by Pulsed HF-heating Gennady Milikh University of Maryland PARS-2 Workshop, November 3 – 6, 2002.
Chapter 4 Waves in Plasmas 4.1 Representation of Waves 4.2 Group velocity 4.3 Plasma Oscillations 4.4 Electron Plasma Waves 4.5 Sound Waves 4.6 Ion Waves.
Which describes a variation of wave frequency ω(t) in a geometric-optic approximation [4]. Here n(ω) is the refractive index of the medium, is the vector.
Modeling Generation and Nonlinear Evolution of VLF Waves for Space Applications W.A. Scales Center of Space Science and Engineering Research Virginia Tech.
Modeling Generation and Nonlinear Evolution of Plasma Turbulence for Radiation Belt Remediation Center for Space Science & Engineering Research Virginia.
Nonlinear Evolution of Whistler Turbulence W.A. Scales, J.J. Wang, and O. Chang Center of Space Science and Engineering Research Virginia Tech L. Rudakov,
1 Duct Formation by HF heating Gennady Milikh, Aram Vartanyan, Dennis Papadopoulos, University of Maryland Evgenii Mishin, Air Force Research Lab, Hanscom.
Subionospheric VLF propagation
Generation of intense quasistatic fields at high altitudes by the Ionospheric Alfvén Resonator Bill Lotko, Jon Watts, Anatoly Streltsov Thayer School of.
Damping of Whistler Waves through Mode Conversion to Lower Hybrid Waves in the Ionosphere X. Shao, Bengt Eliasson, A. S. Sharma, K. Papadopoulos, G. Milikh.
Terrestrial gamma-ray flashes Prepared by Morris Cohen Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network.
1 Particle-In-Cell Monte Carlo simulations of a radiation driven plasma Marc van der Velden, Wouter Brok, Vadim Banine, Joost van der Mullen, Gerrit Kroesen.
Satellite observation systems and reference systems (ae4-e01) Signal Propagation E. Schrama.
1 Sferics and Tweeks Prepared by Ryan Said and Morris Cohen Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME.
Why does the temperature of the Sun’s atmosphere increase with height? Evidence strongly suggests that magnetic waves carry energy into the chromosphere.
Dipole antenna: Experiment/theory status Timothy W. Chevalier Umran S. Inan Timothy F. Bell February 18, 2009.
Finite Temperature Effects on VLF-Induced Precipitation Praj Kulkarni, U.S. Inan and T. F. Bell MURI Review February 18, 2009.
Naval Weapons Systems Energy Fundamentals Learning Objectives  Comprehend basic communication theory, electromagnetic (EM) wave theory  Comprehend.
Whistler Wave Launch and Diamagnetic Plasma Formation in Laboratory Experiments Bill H. Quon, Microwave Plasma Applications 252 S. Poplar Ave # 403 Brea,
Magnetospheric Morphology Prepared by Prajwal Kulkarni and Naoshin Haque Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global.
Electromagnetic Wave Theory
V. M. Sorokin, V.M. Chmyrev, A. K. Yaschenko and M. Hayakawa Strong DC electric field formation in the ionosphere over typhoon and earthquake regions V.
Ionospheric Absorption Prepared by Forrest Foust Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network.
RESONANCE Project for Studies of Wave-Particle Interactions in the Inner Magnetosphere Anatoly Petrukovich and Resonance team RESONANCEРЕЗОНАНС R.
Consider a time dependent electric field E(t) acting on a metal. Take the case when the wavelength of the field is large compared to the electron mean.
Nonlinear VLF Wave Physics in the Radiation Belts Chris Crabtree Guru Ganguli Erik Tejero Naval Research Laboratory Leonid Rudakov Icarus Research Inc.
1 Association Euratom-Cea TORE SUPRA Tore Supra “Fast Particles” Experiments LH SOL Generated Fast Particles Meeting Association Euratom IPP.CR, Prague.
Lecture 2: Antennas and Propagation Anders Västberg
Physics and Measurements of Stimulated Electromagnetic Emissions Paul A. Bernhardt, Stan Briczinski Plasma Physics Division Naval Research Laboratory.
Remote Radio Sounding Science For JIMO J. L. Green, B. W. Reinisch, P. Song, S. F. Fung, R. F. Benson, W. W. L. Taylor, J. F. Cooper, L. Garcia, D. Gallagher,
N. Yugami, Utsunomiya University, Japan Generation of Short Electromagnetic Wave via Laser Plasma Interaction Experiments US-Japan Workshop on Heavy Ion.
Current Drive for FIRE AT-Mode T.K. Mau University of California, San Diego Workshop on Physics Issues for FIRE May 1-3, 2000 Princeton Plasma Physics.
Space Science MO&DA Programs - September Page 1 SS It is known that the aurora is created by intense electron beams which impact the upper atmosphere.
UPenn NROTC Unit, dtd Fall 2004 Naval Weapons Systems Energy Fundamentals.
Fyzika tokamaků1: Úvod, opakování1 Tokamak Physics Jan Mlynář 8. Heating and current drive Neutral beam heating and current drive,... to be continued.
Spatial Effects of Multiple Scattering of HF Signals in the Ionosphere: Theory and Experiment N. Zabotin 1,2, J.W. Wright 2, A. Gasiewski 1, G. Zhbankov.
Surface Plasmon Resonance
1 On remote sensing of TLEs by ELF/VLF wave measurements on board a satellite F. Lefeuvre 1, R. Marshall 2, J.L. Pinçon 1, U.S. Inan 2, D. Lagoutte 1,
XVII CLUSTER Workshop, Uppsala, 14 May 2009 Fan and horseshoe instabilities -relation to the low frequency waves registered by Cluster in the polar cusp.
Physics 1202: Lecture 18 Today’s Agenda Announcements: –Lectures posted on: –HW assignments, etc.
Outline Motivation and observation The wave code solves a collisional Hall-MHD model based on Faraday’s and Ampere’s laws respectively, coupled with.
Whistler Waves and Related Magnetospheric Phenomena
Laboratory Experiments on the interaction of electromagnetic waves at plasma gradients Walter Gekelman Pat Pribyl Yuhou Wang* * Left for position at LAM.
A. Vaivads, M. André, S. Buchert, N. Cornilleau-Wehrlin, A. Eriksson, A. Fazakerley, Y. Khotyaintsev, B. Lavraud, C. Mouikis, T. Phan, B. N. Rogers, J.-E.
Laboratory Study of Spiky Potential Structures Associated with Multi- Harmonic EIC Waves Robert L. Merlino and Su-Hyun Kim University of Iowa Guru Ganguli.
Phonons Packets of sound found present in the lattice as it vibrates … but the lattice vibration cannot be heard. Unlike static lattice model , which.
Ionospheric HF radars Pasha Ponomarenko. Outline Conventional radars vs ionospheric radars Collective scatter processes Aspect angle effects HF propagation.
Integrity  Service  Excellence Physics of the Geospace Response to Powerful HF Radio Waves HAARP-Resonance Workshop, 8-9 November 2011 Evgeny Mishin.
1.1 What’s electromagnetic radiation
Large Area Plasma Processing System (LAPPS) R. F. Fernsler, W. M. Manheimer, R. A. Meger, D. P. Murphy, D. Leonhardt, R. E. Pechacek, S. G. Walton and.
Numerical simulations of wave/particle interactions in inhomogeneous auroral plasmas Vincent Génot (IRAP/UPS/CNRS, Toulouse) F. Mottez (LUTH/CNRS, Meudon)
5.4 Stored Energy Crashes  Diamagnetic loop shows the plasma energy crashes at low plasma density  ECE signals are in phase with the energy crashes 
Laser target interactions, and space/solar physics simulation experiments (Seed funding project) Laser-target: Boris Breizman, Alex Arefiev, Mykhailo Formyts'kyi.
By Saneeju m salu. Radio waves are one form of electromagnetic radiation RADIO WAVES.
The Role of VLF Transmitters in Limiting the Earthward Penetration of Ultra-Relativistic Electrons in the Radiation Belts J. C. Foster, D. N. Baker, P.J.
1 1 Office of Science Strong Field Electrodynamics of Thin Foils S. S. Bulanov Lawrence Berkeley National Laboratory, Berkeley, CA We acknowledge support.
Evolution of the poloidal Alfven waves in 3D dipole geometry Jiwon Choi and Dong-Hun Lee School of Space Research, Kyung Hee University 5 th East-Asia.
Chapter 8 Antennas Propagation Dave Piersall, N6ORB.
JongGab Jo, H. Y. Lee, Y. H. An, K. J. Chung and Y. S. Hwang*
Sky Wave Propagation.
Introduction to Atmospheric Science at Arecibo Observatory
Simulations of Ionospheric Turbulence near the Upper Hybrid Layer
Earth’s Ionosphere Lecture 13
Energy conversion boundaries
The Ionosphere Equatorial Anomaly.
Three Regions of Auroral Acceleration
Presentation transcript:

PARS Workshop on Novel Methods of Excitation of ULF/ELF/VLF to Improve Efficiency and Availability" November 3 - 6, 2002 Sponsored by Air Force Research Laboratory, Office of Naval Research University of Alaska, Fairbanks Institute of Plasma Science and Technology, UCLA Arrowhead Conference Center

Goals and Objectives 1.Review experiments on EM interactions with Ionosphere leading to ULF/ELF/VLF (UEV) 2. Efficient Generation of waves with and without electrojet Examine New Approaches High power EM pulses at HF and Laser frequencies 3. Improved methods of Detection 4. Laboratory experiments and Computer Modeling

UEV Physical Pictures. VLF - Whistler waves Accessibility and electron cyclotron resonance. ELF waves – Ion cyclotron waves. ULF waves – Alfven waves.

Whistler waves are accessible for propagating into and heating the high density plasma The RHCP Whistlers can be excited into both low and high density plasma by launching from high magnetic field (  ce /  > 1). These waves do not go across the R- cutoff layer, and pass the L-cutoff without being affected. The accessibility problem arises in the vicinity of the boundary  pe /  = 1. The CMA diagram shows that the RHCP waves propagation along B will pass this boundary, but those perpendicular to B will be reflected.

The LHCP ion cyclotron waves are similar to the RHCP electron whistler waves. They can be excited using a dipole loop antenna inside the plasma. Excitation LHCP Ion Cyclotron Waves by Modulation of the Diamagnetic Dipole at ELF/VLF with AM HF Power. Densi ty

Electrons can be heated by electromagnetic waves near the electron cyclotron resonant zone For whistler waves, the resonance condition requires  -  ce - k z v z  0 Strong absorption occurs for those electrons moving backwards k z v z  (  -  ce ) < 0. ECR condition:    ce in uniform B.

Alfven Wave B 1, v 1, E 1, J 1

ELF/VLF Excitation by Pulsed HF Power at the Electron Cyclotron Resonance 1.Accelerate electrons to ionizing energy using pulsed HF ECR power. 2.Production of high density plasma by impact ionization. 3.Formation of diamagnetic plasma disk by multiple pulses of HF power. 4.Modulation of diamagnetic plasma by electron heating using CW HF power modulated at ULF/ELF/VLF range. 5.Excitation of Low frequency Whistler modes and ion cyclotron waves to further enhance the ULF/ELF/VLF signals. Our goal is to generate a large plasma magnetic dipole moment below or above 100 km above HIPAS. The ELF/VLF magnetic field produced can be sensed around the world through the earth-ionosphere-waveguide. Alfven Wave

Plasma Diamagnetic Current J  = c BX  p/B 2 I  =  dz  dr J  Magnetic Dipole Moment m =  a 2 I  /c  nT  V/B L A plasma with electron density n=1x m -3 T e = 1 eV and L= 3 km; r=10 km; p= n  T = 1x10 11 eV m -3 Diamagnetic Current Carried by the Plasma: I = 1 A Magnetic Dipole Moment: m =  r 2 I = 3.14 x 10 8 A-m 2 p JJ Localized Plasma produced by HF ECR Carried Magnetic Dipole Moment The objective of an active ionosphere modification is to increase and modulate the diamagnetic dipole moment at the ELF/VLF by HF radiation from ground.

Plasma current produced by HF wave heating can generate significant ELF/VLF radiation signals r  m =  a 2 I/c Magnetic field of magnetic dipole moment: B r = 2 m cos  /r 3 B  = m sin  /r 3 For I = 100A, a = 10 km, the magnetic field induction at 100 km from the dipole ring is about 6.3 pT. Higher ELF/VLF signal levels are expected from collective plasma oscillations and reflection from the ionosphere (the earth-ionosphere waveguide effect). 100 km 3.6 pT 6.3 pT I = 100A a = 10 km

The RHCP wave power is completely absorbed at the ECR zone while the LHCP wave is reflected at the L-Cutoff boundary Ray tracing for the electromagnetic waves satisfying the Appleton Hartree dispersion relation >p>p >p>p <p<p <p<p RHCP LHCP

Whistler wave ducting by a low plasma density trough will effectively increase the HF power flux at the target region Experimental demonstration of the unducted and ducted Whistler waves.

Whistler Wave Propagation and Absorption Index of Refraction (n = ck/  ) n 2 = 1 +  p 2 /  2 / [(  ce /  ) cos  -1] Wave Absorption k i = - D i /(  D/  k) =  p 2 /(2c 2 k 2 v e )  EXP{-[(  -  ce )/kv e ] 2 } P abs = {1- exp [-2⌠k i (x)dx]} P Resonance Length L res : Length of layer with: 1% < P aps /P < 99%

Whistler Wave Propagation and Absorption In the Ionosphere 100 km Index of refraction Imaginary wavenumber Wave Amplitude Waveform The absorption layer for the electron whistler is typically 2-3 kilometer thick.

Electron Heating by Electron Whistler Wave Against Electron-Neutral Collisions Electron heating in single pass of electron Cyclotron Resonance: E = (Z o /(ck/  )*P/A) 1/2  = Min (  e-n,  res,  0 )  v = e/m E  T  = ½ e 2 /mE 2  2  e-n = sec (collision)  res = sec (Resonance)  0 = sec (Pulse) The electron-neutral collision time  e-n  sec at about 100 km altitude in the E-layer where the normal electron temperature is cold, Te = 0.03 eV (300 K). The electrons must gain enough energy (T  > 20 eV) in a time short compared to  e-n such to minimize excitation energy loss. It requires about 20 mW/m 2 of the HF power flux to bring the electrons to the ionizing energy level by electron cyclotron resonance heating in the ECR layer.

Pulsed HF Power Will be Used for Electron Accelerations Frequency: f = 1.4 MHz Plasma Parameters n e = cm -3 Vacuum Electric Field E o = 4 V/m (  = 128 mW/m 2 ) Refraction Index n = 3.4 Plasma Heating Field E = 4.3 V/m Minimum Collision Time:  min  1 x sec. Energy Gain (per pass) T  = 46.9 eV The 4 V/m electric field requires a power flux,  = 21.3 mW/m 2, or 2.7 GW ERP. This power level will be available from pulsed transmitters currently under development at HIPAS Observatory.

Creating High Density Plasma by electron Impact Ionizations The energetic electrons created by HF ECR are capable of ionizing the background neutral particles in a fast time scale, I.e sec. Plasma produced will be localized in the heating region for a time scale of electron-ion recombination time, I.e. ~100 sec. Thus a very high density plasma can be created using multiple HF pulses in a time scale of the recombination time.

Areas of Further Investigation and Preparation for HIPAS Active Ionospheric Modification Experiments 1.Study the wave propagation and wave-particle interactions using realistic 3D PIC simulations 2.Understanding the detailed electron heating and diamagnetic plasma formation process using laboratory modeling experiments with relevant scaling parameters. 3.Detailed power balance including excitation energy losses 4.Develop techniques for charging and discharging the high power pulsed antenna array.

Van Zeeland et al. PRL 2002.