solar physics course lecture art poland modeling mhd equations and spectroscopy
TRANSCRIPT
Why
• What I am going to talk about should lead to our understanding of physical processes in outer solar atmosphere:– Heating– Energy transport– Solar wind acceleration– Magnetic field evolution
Overview• Modeling features in the solar atmosphere
involves solving the full MHD equations.
• The solution of these equations needs initial conditions and boundary conditions.
• To get realistic values, you need observations.
• In this lecture I will first talk about how to get the observations, and then how they are used in the solution of the equations.
What Quantities Do We Need?
• The equations tell us we need to observe– Temperature– Density– Velocity– Magnetic field
• To do time dependence we need each as a function of time.
Questions
• How can we measure these quantities at the Sun?
• Spectroscopic observations
• What causes an absorbtion line? How is one formed?
• Why are some lines in emission?
Comments
• Equations derived from observations in the lab. of atomic spectra.
• Quantum mechanics gives more precise description.
• What I am showing helps visualize the structure.
Level Splitting, Momentum
• When there are multiple electrons in an atom, the n levels are split.
• The split levels are referred to as s,p,d,f,– For n=1 there are only s levels– For n=2 there are s and p levels– For n=3 there are s,p,and d levels– etc
Spin• The other quantity is electron spin.
– He for example has 2 electrons, both can occupy the n=1 level because one has a spin of +1/2 and the other a spin of -1/2
– Transitions between spin level have a very low probability, and are referred to as forbidden transitions.
– When they are opposite to each other they are referred to as singlets
– When they are the same, triplets– Spin combined with momentum can also give
doublets.
Sample Energy Diagram
• Allowed transitions
• Forbidden transitions
• Magnetic fields can split sub-levels (ie 22s into 2 levels).
Summary
• Atomic structure - Spectral lines
• Electron transitions– N levels– Momentum s,p,d,f– Spin
• Momentum and spin splitting occurs in magnetic field – can use splitting to measure strength of field.
How to Use Spectra
• Velocity?– Doppler shift– Sometimes just an asymmetry in profile
• What else?
• Temperature – next topic
• Density – next topic
Gas State
• 1) The basic observed equation is P=NkT, N=ρ/uMH – a. This is important: if you know two, you know the third. – b. Can make observations that yield T, and ρ so you can get P.
• 2) Temperature and mean velocity – visualization again– a. Perfect box with perfect collisions: collision momentum with
wall is 2mvx – b. Number of collisions vx/2L L is size of box – c. Total of all momentum is ΣΜvx
2/L – d. Momentum is pressure so P=ML-3Σvx
2 – e. Define mean vx
2=n-1Σvx2
– f. vx2=vy
2=vz2=1/3v2
– g. P=n/3L3(Mv2)=1/3(NMv2) – h. So average energy ½ Mv2=3/2 kT This is important because it
relates energy, velocity, to temperature. (not bulk velocity)
Get The T• Velocity of atoms and electrons related to T was
just shown.• What do we need to get the temperature of the
gas? First assumption?– Assume a Maxwellian velocity distribution
• What must be assumed for this to be valid?– Collisions (not so good at very low
• f(v,T)= (M/2πkT)3/2v2e-(Mv2/2kT)
• Maxwellian tail of distribution
Boltzmann Distribution• a. Ni/N=gi/ue-ε/kT ε=hν
• b. Can use the ratio for 2 energy levels to get relative populations between two energy levels.
• c. Measure two lines from same atom to get T
• d. Ni/Nj=gi/gje-δε/kT
Saha Equation
• a. equation of ionization state:
• Ni/Nj(Ne)=(2πmkT)3/2/h3(2(ui(T)/uj(T))e-ε/kT
• b. Used to determine gas temperature
N
T
FeIII FeIV
How to Get Lines
deSI )τ()( ν
0
– I is the intensity you observe– S is emission/cm3
is optical depthis frequency– How do you get an absorption line from this?– How do you get an emission line?
Other issues
• Non-LTE
• A or f values– Line brightness– Collision prob.
• Plank function
• Differential emission measure
Log Ne2
Summary
• Spectra can give us:– T via line width, line ratios– Density via line ratios or diff. emission
measure– Velocity via line shift
How to Solve
• Depends on the problem– Near the Sun small area, cartesian – Whole Sun or Heliosphere, spherical
• Coupled differential equations.• The big problem is steep gradients.
– Transition region (T gradient)– Flares (P gradients, shocks)
• The boundary conditions you choose almost always dictate the solution.
Results
• The output of these programs are table of numbers, T(x,y,z,t), P(x,y,z,t),etc.
• Need to visualize the results
• Need to make visualizations something that you can compare with observations.
Variable Grid MeshMajor Breakthrough
• Paramesh
• Steep T gradient in transition region.
• Almost no gradient in corona.
Other Issues
• Conduction– Isotropic– Anisotropic –along B field
• Radiative losses– Optically thin - collisions– Non-LTE T(collision) T(radiation)
• Heating– Constant– Alfven waves – a function of B
• Make each of these a replaceable module in your program.
Conduction• Conduction only along B field
– How the grid is oriented with respect to B
Excess heating low down
Numerical diffusion makes it wider.