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

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

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LEP Event Properties 3 1.Onset delay (∆t ~ 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 ~ s

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

Atmospheric Chemistry

Prepared by Benjamin CottsStanford University, Stanford, CA

IHY Workshop on Advancing VLF through the Global AWESOME

Network

Page 2: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Overview

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

Page 3: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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 (td ~ 1-2 s) of secondary ionization

4. Large ionospheric region of disturbance, ~ 2000 km

5. Occur very frequently6. Recovery typically ~ 10-100 s

Page 4: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Recovery Signatures of LEP

4Pasko and Inan, 1994Peter 2007

Page 5: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Early VLF Event Properties

Rapid onset delay (t < 20 ms)

Rapid onset duration (td < 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 kmSource: [Johnson and Inan 1999]

Page 6: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Long Recovery Early/fast Events

Page 7: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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

Page 8: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Massive Gamma-Ray Burst

From Inan et al. 2007

Page 9: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Second Timescale Characteristics

From Inan et al. 2007

-25 dB

disturbance!!

From Inan et al. 2007

Page 10: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Hour Timescale Characteristic

From Inan et al. 2007

Recovery lasts

for over 1 hour!

Page 11: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Overview

Ionospheric chemistry• Model Framework• Constituents/Parameters

Page 12: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

Chemistry Model: Species

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• Ne - Electrons• N+ - Light positive ions• Nx

+ - Heavy positive ions (cluster)• N - Light negative ions• Nx

- Heavy negative ions (cluster)

Not part of the model, just illustrative:

Page 13: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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- attachment: - detachment from light

negative ionsx - detachment from heavy

negative ionsi - mutual neutralizationd, d

c - dissociative recombination

A - rate of conversion N Nx

B - rate of conversion N+ Nx+

Page 14: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Model of Ionospheric Chemistry

5 constituents:• Ne - electrons• N+ - light positive ions O2

+, NO2+, N2

+, …• Nx

+ - positive ion clusters H+(H2O)n

• N - light negative ions O, O2, …

• Nx - heavy negative ions NO3

, NO3(H2O)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, Nac: O, N, O2(a1g)

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+ Nx+

A - rate of conversion N Nx

Q – Ionization source; Cosmic ray only source at low altitudes Qcr (peaks at ~15 km)

Page 15: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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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 ~ (iNi)1 ~ 104 s

Page 16: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Gamma-Ray Burst

• Ionization profile recovery

Page 17: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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Page 18: Atmospheric Chemistry Prepared by Benjamin Cotts Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global AWESOME Network

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