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Ion Equatorial Distributions from Energetic Neutral Atom Images Obtained From IMAGE during Geomagnetic Storms. Zhang, X. X., J. D. Perez, M.-C. Fok D. G. Mitchell, C. J. Pollock and X. Y. Wang. Outline. Introduction Image Inversion techniques
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Ion Equatorial Distributions from Energetic Neutral Atom Images Obtained From IMAGE during Geomagnetic Storms Zhang, X. X., J. D. Perez, M.-C. Fok D. G. Mitchell, C. J. Pollock and X. Y. Wang
Outline • Introduction • Image Inversion techniques • Ion equatorial distributions deconvolved from ENA images. • Comparisons b/w deconvolved results and Simulation • T89 and T96 magnetic field model • Discussion and summary
Introduction • What are Energetic Neutral Atoms (ENAs)? • Where are ENA Sources come from? • Why are ENAs so important? • How to get ENA flux? • How to extract the parent ion information from the ENA flux
What are ENAs? Neutral Atoms (ENAs) are generated when single charged ions interact with neutral particles via charge-exchange collisions. Ex: H+ + H H + H+ O+ + H O + H+
Where are ENA Sources ? Whenever energetic charged particles interact or coexist with neutral sources, ENAs are produced. • The hemispheric ENA • Planetary magnetospheres • Laboratory plasma ENAS mainly comes from inner magnetosphere or Ring Current region
Why are ENAs so important? • Specific Energetic neutrals overcomes planetary escaping energy (> 0.6eV/nucleon) • ENA s are not affected by E and B fields • ENAs travel in approximately straight line from the charge-exchange sites • ENAs carry with important information of energy, composition, PAD and directions of source ion distributions
How to get ENA flux? ENA Imaging Optical Imaging • The emission sites are optically thin • The neutral background likes a screen • The ENAs can be imaged to form a 2-D image, not 3-D image. • High altitude imaging better than low altitude
ENA image and deconvolution • ENA images from MENA HENA: fisheye • Deconvolved ion flux from ENA images * Ion distributions * Pitch angle anisotropy
How to extract ion information from ENA Image • Forward modeling techniques * A set of parameters keeps updating * Theoretical and empirical models * matching simulated image • Image inversion techniques * Base on actual ENA image data * A set of linear spatial expansion/spline * smooth and fitting the data by minimizing 2
Deconvolution techniques • Developed and improved by Dr. Perez and also applied to simulated data and IMAGE ENA data
Deconvolution from ENA • Ion distributions deconvolved from actual ENA images by expanding ion flux distribution in term of 3-cubic splines. • Requiring: * fit the data by minimizing 2 =1 * smooth the data using smallest 2nd derivatives of ion flux distributions.
New features • The response function of instrument (new) • Charge-exchange with • Hydrogen geocorona • Oxygen in the exosphere (new) * Exobase density derived from MSISE 90 * Solar radio flux parameters, (1) F107a 3-month average (2) F107 previous day’s value (3) Ap daily average
Important and needed • HENA response function obtained from Bob Demajistre (APL) • HENA data extraction code from Pontus C:Son Brandt (APL) • MENA data extraction code from Joerg-Micha Jahn (SWRI)
Ion equatorial distributions from ENA images. • Case 1: Ion distributions dependence on Energies (Aug. 12, 2000) • Case 2: Ion distribution drifting(June 10, 2000) • Case 3: Ring current structures and ion distribution patterns • Case 4: Ion flux decay and intensify
Ion distributions via Energies • Ion distributions from MENA and HENA images on Aug. 12, 2000 at time 1100UT • The ion fluxes from MENA and HENA show their different source locations, * pre-midnight for lower energies (MENA) * post-midnight for higher energies (HENA) * the flux intensity drops from low energy to high energy
Ion distributions via drift • Ion distributions from MENA and HENA images on June 10, 2000 at different time • The ion fluxes from MENA and HENA show their different azimuthal drifts, * small drift for lower energy (MENA) * drift west for higher energy (HENA) • Drift=E+gradient+curvature+co-rotation
Ion distributions via symmetry • Ion distributions from MENA and HENA images on June 10 and Oct. 4, 2000 • The ion fluxes from MENA and HENA show different ring current patterns/ring current structures * (MENA) * (HENA)
Ion flux evolving and decaying Ion flux intensity variations from MENA on Aug. 12, 2000. (solar wind plasma and IMF) • drops at the end of main phase • decay rapidly at the initial recovery phase • Intensify at the time of turning direction of Bz • Round 1400, substorms contribute and intensify the ion fluxes but ENA did not show intense • Dst, AE, ASY, SYM
Deconvolutions via Simulations • What are physics in them? Substorm/electric field convection • Most large scale structures exist in both Deconvolutions and simulations • There also have some differences.
Discussion and summary • Equatorial ion flux and PAD distributions can be extracted from ENA images. • Deconvolutions show agreements with Fok’s ring current model for most large scale structures. Substorm injections intensify the ion fluxes and ENA flux. • Different energies, phase, and IMF show different ion flux distributions and PADs • The ion fluxes show symmetric and asymmetric ring structures