1. ESS 154/200C Lecture 17 The Auroral Ionosphere

2. Date Day Topic Instructor Due
ESS 200C Space Plasma Physics ESS 154 Solar Terrestrial Physics M/W/F 10:00 – 11:15 AM Geology Instructors: C.T. Russell (Tel. x-53188; Office: Slichter 6869) R.J. Strangeway (Tel. x-66247; Office: Slichter 6869)
Date Day Topic Instructor Due
1/4 M A Brief History of Solar Terrestrial Physics CTR
1/6 W Upper Atmosphere / Ionosphere CTR
1/8 F The Sun: Core to Chromosphere CTR
1/11 M The Corona, Solar Cycle, Solar Activity
Coronal Mass Ejections, and Flares CTR PS1
1/13 W The Solar Wind and Heliosphere, Part 1 CTR
1/15 F The Solar Wind and Heliosphere, Part 2 CTR
1/20 W Physics of Plasmas RJS PS2
1/22 F MHD including Waves RJS
1/25 M Solar Wind Interactions: Magnetized Planets YM PS3
1/27 W Solar Wind Interactions: Unmagnetized Planets YM
1/29 F Collisionless Shocks CTR
2/1 M Mid-Term PS4
2/3 W Solar Wind Magnetosphere Coupling I CTR
2/5 F Solar Wind Magnetosphere Coupling II;
The Inner Magnetosphere I CTR
2/8 M The Inner Magnetosphere II CTR PS5
2/10 W Planetary Magnetospheres CTR
2/12 F The Auroral Ionosphere RJS
2/17 W Waves in Plasmas 1 RJS PS6
2/19 F Waves in Plasmas 2 RJS
2/26 F Review CTR/RJS PS7
2/29 M Final

3. Auroral Dynamics

4. Auroral Rays
Auroral Rays from Ground Auroral Rays from Space Shuttle
Auroral emissions line up along the Earth’s magnetic field because the causative energetic particles are charged.
The rays extend far upward from about 100 km altitude and vary in intensity.

5. Auroras Seen from High Altitude
From 1000 km (90m orbit) From 4RE on DE-1
Auroras occur in a broad latitudinal band; these are diffuse aurora and auroral arcs; auroras are dynamic and change from pass to pass.
Auroras occur at all local times and can be seen over the polar cap.

6. Auroral Spectrum
Auroral light consists of a number discrete wavelengths corresponding to different atoms and molecules
The precipitating particles that cause the aurora varies in energy and flux around the auroral oval

7. Exciting Auroral Emissions
Electron impact: e+N→N*+e1
Energy transfer: x*+N→x+N*
Chemiluminescence: M+xN→Mx*+N
Cascading: N**→N*+hν
(N2+)*→N nm(uν) or 427.8nm (violet) aurora
O(3P)+e→O(1S)+e′
O(1S)→O(1D)+557.7nm (green line)
O(1D) →O(3P)+630/636.4nm (red line)
Forbidden lines have low probability and may be de-excited by collisions.
1D, t=110 s
Energy levels of oxygen atom

8. Auroral Emissions
Protons can charge exchange with hydrogen and the fast neutral moves across field lines.
Precipitating protons can excite Hα (656.3nm, red) and Hβ (486.1 nm, cyan) emissions and ionize atoms and molecules.
Day time auroras are higher and less intense.
Night time auroras are lower and more intense.
Aurora generally become redder at high altitudes.
red
magenta
green

9. The Aurora – Colors

10. Auroral Forms Forms Homogenous arc Arc with rays Homogenous band
Band with rays
Rays, corona, drapery
Precipitating particles may come down all across the auroral oval with extra intensity/flux in narrow regions where bright auroras are seen.
Visible aurora correspond to energy flux of 1 erg cm-2s-1.
(1 mw/m2), or 1 kR
Nadir Pointing Photometer Observations

11. Height Distribution/Latitude Distribution
Auroras seen mainly from km
Top of auroras range to over 1000km
Aurora oval size varies
from event to event
during a single substorm

12. Polar Cap Aurora
Auroras are associated with field-aligned currents and velocity shears.
The polar cap may be dark but that does not mean field lines are open.
Polar cap aurora are often seen with strong interplanetary northward magnetic field

13. Auroral Substorm Growth phase – energy stored
Model based on ground observations Pictures from space
Growth phase – energy stored
Onset – energy begins to be released
Expansion – activity spreads

14. Conductivity Parallel equation of motion
Perpendicular equation of motion
Conductivity tensor
Pedersen conductivity (along E┴)
Hall conductivity (along -E x B)
Parallel conductivity

15. Auroral Currents
If collisions absent then electric field produces drift perpendicular to B.
When collisions occur at a rate similar to the gyrofrequency drift is at an angle to the electric field
If B along Z and conductivity strip along x, we may build up charge along north and south edge and cut off current in north-south direction. If
Called the Cowling conductivity

16. Magnetosphere Ionosphere Coupling
Magnetosphere can transfer momentum to the ionosphere by field-aligned current systems.
Ionosphere in turn can transfer momentum to atmosphere via collisions.
Magnetosphere can heat the ionosphere.
Magnetosphere can produce ionization.
Ionosphere supplies mass to the magnetosphere.
Process is very complex and is still being sorted out.

17. Force Balance - MI Coupling

18. Maxwell Stress and Poynting Flux

19. Currents and Ionospheric Drag

20. Weimer FAC morphology

21. FAST Observations IMF By ~ -9 nT.
IMF Bz weakly negative, going positive.

22. Three Types of Aurora Auroral zone crossing shows:
Inverted-V electrons (upward current)
Return current (downward current)
Boundary layer electrons
(This and following figures courtesy C. W. Carlson.)

23. Upward Current – Inverted V Aurora

24. Downward Current – Upward Electrons

25. Polar Cap Boundary – Alfvén Aurora

26. Primary Auroral Current
Inverted-V electrons appear to be primary (upward) auroral current carriers.
Inverted-V electrons most clearly related to large-scale parallel electric fields – the “Knight” relation.

27. Current Density – Flux in the Loss-Cone
The auroral current is carried by the particles in the loss-cone.
Without any additional acceleration the current carried by the electrons is the precipitating flux at the atmosphere:
j0 = nevT/2p1/2 ≈ 1 mA/m2 for n = 1 cm-3, Te = 1 keV.
A parallel electric field can increase this flux by increasing the flux in the loss-cone. Maximum flux is given by the flux at the top of the acceleration region (j0) times the magnetic field ratio (flux conservation - with no particles reflected).
jm = nevT/2p1/2  (BI/Bm).

28. Asymptotic Value = BI /Bm
Knight Relation
The Knight relation comes from Liouville’s theorem and acceleration through a field-aligned electrostatic potential in a converging magnetic field.
Does not explain how potential is established.
1+e/T
Asymptotic Value = BI /Bm
j/j0
e/T
[Knight, PSS, 21, , 1973; Lyons, 1980]

29. Auroral Kilometric Radiation - Horseshoe Distribution
Strangeway et al., Phys. Chem. Earth (C), 26, , 2001.