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Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network.

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Presentation on theme: "Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network."— Presentation transcript:

1 Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

2 Overview  LEP Events  Early/fast Events  Gamma Ray Burst (GRB) Events  Atmospheric Chemistry

3 LEP Event Properties 3 1.Onset delay (∆t ~ 0.5-2 s) between sferic and onset 2.Differential onset delay with respect to L-shell (~0.5s) 3.Onset duration (t d ~ 1-2 s) of secondary ionization 4.Large ionospheric region of disturbance, ~ 2000 km 5.Occur very frequently 6.Recovery typically ~ 10-100 s

4 Recovery Signatures of LEP 4 Pasko and Inan, 1994Peter 2007

5 5 Early VLF Event Properties  Rapid onset delay (  t < 20 ms)  Rapid onset duration (t d < 20 ms)  Typically recover in ~30-200 s  Event amplitudes ~0.2 - 0.8 dB, rarely >1 dB  Causative CGs <50 km from perturbed path  Lateral extent of disturbances ~100 km Source: [Johnson and Inan 1999]

6 6 Long Recovery Early/fast Events

7 Gamma-Ray Bursts  Associated with very energetic explosions Collision of Neutron stars Magnetar  Typically lasts a few ms to several minutes  Accidentally discovered by Vela-3 spacecraft in 1967

8 Massive Gamma-Ray Burst From Inan et al. 2007

9 Second Timescale Characteristics From Inan et al. 2007 -25 dB disturbance!! From Inan et al. 2007

10 Hour Timescale Characteristic From Inan et al. 2007 Recovery lasts for over 1 hour!

11 11 Overview  Ionospheric chemistry Model Framework Constituents/Parameters

12 Chemistry Model: Species 12 N e - Electrons N + - Light positive ions N x + - Heavy positive ions (cluster) N  - Light negative ions N x  - Heavy negative ions (cluster) Not part of the model, just illustrative:

13 13  - attachment:  - detachment from light negative ions  x - detachment from heavy negative ions  i - mutual neutralization  d,  d c - dissociative recombination A - rate of conversion N   N x  B - rate of conversion N +  N x +

14 14 Model of Ionospheric Chemistry  5 constituents: N e - electrons N + - light positive ions O 2 +, NO 2 +, N 2 +, … N x + - positive ion clusters H + (H 2 O) n N  - light negative ions O , O 2 , … N x  - heavy negative ions NO 3 , NO 3  (H 2 O) n Coefficients:   i - mutual neutralization   d,  d c - dissociative recombination   - attachment: 3-body and 2-body (in E)   - detachment from light negative ions (value uncertain): Electron affinity=0.4 eV  highly dependent on T During daytime: photodetachment=0.4 s -1 Also due to active species, N ac : O, N, O 2 (a 1  g )   x - detachment from heavy negative ions, approximately=0 (electron affinity = 3.91 eV), photodetachment = 0.002 s -1 (during daytime)  B - rate of conversion N +  N x +  A - rate of conversion N   N x   Q – Ionization source; Cosmic ray only source at low altitudes Q cr (peaks at ~15 km)

15 15 Inan et al., 2007 Recall Gamma-Ray Burst Relaxation matches model results, 2 stages: –Free electrons are quickly attached,  1 ~ (  +   1 –Positive and negative ions recombine,  2 ~ (  i N i )  1 ~ 10 4 s

16 16 Gamma-Ray Burst Ionization profile recovery

17 17

18 Bibliography  Mitra, A. P. 1975  Ferguson, 1979  Arijs, 1992  Glukhov et al., 1992  Pasko and Inan, 1994  Rodger et al., 1998  Inan et al., 2007  Lehtinen and Inan, 2007


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