ask observations and modelling of n 2 first positive emission in aurora – ii . cross sections
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ASK observations and modelling of N 2 first positive emission in aurora – II . Cross sections Joanna Sullivan (presenter) Mina Ashrafi Betty Lanchester Dirk Lummerzheim Nickolay Ivchenko O. Jokiaho D. Whiter ASK workshop Stockholm, June 2008. 20 18 16 14 12 10. N 2. - PowerPoint PPT PresentationTRANSCRIPT
ASK observations and modelling of N2 first positive emission in aurora – II . Cross sections
Joanna Sullivan (presenter) Mina Ashrafi
Betty LanchesterDirk LummerzheimNickolay Ivchenko
O. JokiahoD. Whiter
ASK workshop Stockholm, June 2008
2ASK workshop, Stockholm, June 2008 N2 modelling
• N2 First positive system stems from transition of the B electronic state of the molecular nitrogen to the A state.
• ASK1 filter @ 673.0 nm records two bands of this system: (5,2) and (4,1). (5,2) at 670.4 nm observed intensity in normal aurora is ~18.2 kR and (4,1) at 678.8 nm intensity is ~17.59 kR (Vallance Jones, 1971, Table 4.12)
• N2 1st positive observed total band intensity is 882 kR.
0.4 0.8 1.2 1.6 2.0 2.4 2.8 3.2
20
18 16
14
12
10
8
6
4
2
0
internuclear distance ( )οA
pote
ntia
l ene
rgy
(eV
)
N2
ΠB3
ΣA3
ΣX1(Ground Level)
0
5
0
10
15
5
5
10
10
(5,2) and (4,1) bands
Exc
itatio
n
N2 1st positive system
3ASK workshop, Stockholm, June 2008 N2 modelling
N2 first positive system, 5,200-10,000
(5,2) & (4,1)
Rel
ativ
e sc
ale
0.85
Band transmittance
0.67
ASK1 filter transmission curve
(673.0 nm)
οA
Synthetic spectra (Jokiaho et al., 2008)was used for determining the ASK1 filter
transmission factor (TF):
300 K : TF= 0.76 1000K : TF= 0.66
4ASK workshop, Stockholm, June 2008 N2 modelling
1 minute guide to modelling1 minute guide to modelling
TFF(VJ)IMIA Intensity of N2
measured by ASK1 (calibrated and
background subtracted)
Modelled N2 intensity ( direct + cascading )
"'
)1,4()2,5(
vvIII
Constant determining the contribution from (4,1) and (5,2) bands compare
to the total 1st positive band (V. Jones, 1971):
ASK1 filter transmission factor
Model
Precipitating Electrons energy spectrum
(Maxwellian+mono+powerlaw)
Excitation cross section of atmospheric constituents
N2, O2 , O, etc…
Model Inputs
, … other inputs
5ASK workshop, Stockholm, June 2008 N2 modelling
Ne (
/m3 )
ra
dar d
ata
AS
K1
@ 6
73.0
Inte
nsity
(kR
)
Event Event 22 Oct 200622 Oct 2006
6ASK workshop, Stockholm, June 2008 N2 modelling
ΠC3
ΣB'3
ΣA3
ΠB3ΔW3
ΣX'
1st positive
N2
Ene
rgy
• Nitrogen 1st positive emission intensity measured by ASK includes cascades’
contribution from higher states (B’, C and W) as well as direct excitation of the B
state.
• In order to take into account population of B state resulting from cascades,
modelled population of these higher states were also added to produce output
emission intensities.
7ASK workshop, Stockholm, June 2008 N2 modelling
Cross section for excitation of the N2 B state
Cross section for excitation of the N2
B, C, B’ and W states (R. Link, private communication with D. Lumm.)Cross section for excitation of the N2
B, C, B’ and W states (Itikawa, 2005)
8ASK workshop, Stockholm, June 2008 N2 modelling
Electron impact excitation cross sections of the N2 B statevs. emissions cross sections of the first positive system
A more direct solution for modelling the N21P band intensitymight be to use measured emission cross sections, so that all
cascades are included.
9ASK workshop, Stockholm, June 2008 N2 modelling
Emission cross section of Stanton and St. John produce the best estimate of the N2 emissions.
Uncertainties associated with the reported cross sections could explain the discrepancies between modelled and measured emissions.
Brunger et al. (2003) estimated the uncertainty of up to 35% for B-state cross sections, 30% for B’ and C and 40% for W state. Stanton and St. John estimated a possible systematic error of 18% fortheir emissions cross sections.
ResultsResults
10ASK workshop, Stockholm, June 2008 N2 modelling
Summary and conclusionSummary and conclusion
• Maxwellian and mono-energetic flux and energies are inputs to the model, these are calculated and adjusted using radar and N2 emission intensity.
• Modelled electron densities agree well with the E-region electron density profiles measured by EISCAT radar and therefore the input flux and energy are accurate estimates of the precipitating electron spectrum.
• Excitation cross sections by R. Link and Itikawa (2005) underestimate the N2 first positive intensity by ~30%.
• Emissions cross sections of Shemansky and Broadfoot (1971) overestimates the N2 emission intensity by ~40%.
• Using emissions cross sections of Stanton and St. John (1969) the modelled emission has relatively good agreement with the observed intensities by ASK.
• More accurate and recent cross sections are yet to be found. We will use Stanton and St. John (1969) emissions cross sections for this study.