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(1)

The solar atmosphere

(2)

The Sun’s atmosphere

The solar atmosphere is generally described as being The solar atmosphere is generally described as being composed of multiple layers, with the lowest layer

composed of multiple layers, with the lowest layer being the photosphere, followed by the

being the photosphere, followed by the

chromosphere, the transition region and the corona.

chromosphere, the transition region and the corona.

In its simplest form it is modelled as a single In its simplest form it is modelled as a single component plane-parallel atmosphere.

component plane-parallel atmosphere.

Density drops exponentially: Density drops exponentially: ρρ((zz) ) = = ρρ0 0 exp(-exp(-z/Hz/Hρρ) ) (for (for isothermal atmosphere). T=6000K

isothermal atmosphere). T=6000K  HHρρ≈≈ 100km 100km

Mass of the solar atmosphere Mass of the solar atmosphere ≈≈ mass of the Indian mass of the Indian ocean (

ocean (≈ mass of the photosphere)≈ mass of the photosphere)

Mass of the chromosphere Mass of the chromosphere ≈ mass of the Earth’s ≈ mass of the Earth’s atmosphere

atmosphere

(3)

1-D stratification

(4)

How good is the 1-D approximation?

1-D models reproduce extremely well large parts of 1-D models reproduce extremely well large parts of the spectrum obtained with low spatial resolution the spectrum obtained with low spatial resolution

(see spectral synthesis slide) (see spectral synthesis slide)

However, any high resolution image of the Sun However, any high resolution image of the Sun

shows that its atmosphere has a complex structure shows that its atmosphere has a complex structure

(as seen at almost any wavelength) (as seen at almost any wavelength)

Therefore: 1-D models may well describe averaged Therefore: 1-D models may well describe averaged quantities relatively well, although they probably do quantities relatively well, although they probably do

not describe any part of the real Sun at all.

not describe any part of the real Sun at all.

(5)

The photosphere

The photosphere extends between the solar surface The photosphere extends between the solar surface and the temperature minimum, from which most of and the temperature minimum, from which most of

the solar radiation arises.

the solar radiation arises.

The visible, UV (The visible, UV (λλ> 1600Å) > 1600Å) and IR (< 100and IR (< 100μμm)m) radiation comes from the photosphere.

radiation comes from the photosphere.

4000 K < T(photosphere) < 6000 K4000 K < T(photosphere) < 6000 K

T decreases outwards T decreases outwards  BBνν(T)(T) decreases outwarddecreases outward

 absorption spectrum absorption spectrum

LTE is a good approximationLTE is a good approximation

Energy transport by convection and radiationEnergy transport by convection and radiation

Main structures: Granules, sunspots and faculaeMain structures: Granules, sunspots and faculae

(6)

The Sun in

White Light

(limb darkening

removed)

MDI on

MDI on

SOHO SOHO

(7)

Sunspots

H. Schleicher, KIS/VTT, Obs. del Teide, Tenerife H. Schleicher, KIS/VTT, Obs. del Teide, Tenerife

Umbra

Granule Penumbra

(8)

Granulation

Physics of convection and the properties of Physics of convection and the properties of granulation and supergranulation have been granulation and supergranulation have been

discussed earlier, so that we can skip them discussed earlier, so that we can skip them

here.

here.

(9)

Chromosphere

Layer lying just above the photosphere, at which the Layer lying just above the photosphere, at which the temperature appears to be increasing outwards

temperature appears to be increasing outwards

(classically forming a temperature plateau at around (classically forming a temperature plateau at around

7000 K) 7000 K)

Assumption of LTE breaks downAssumption of LTE breaks down

Energy transport mainly by radiation and wavesEnergy transport mainly by radiation and waves

Assumption of plane parallel atmosphere is very Assumption of plane parallel atmosphere is very likely to break down as well.

likely to break down as well.

Strong evidence for a spatially and temporally Strong evidence for a spatially and temporally

inhomogeneous chromosphere (gas at T<4000K is inhomogeneous chromosphere (gas at T<4000K is

present beside gas with T>8000 K) present beside gas with T>8000 K)

(10)

Chromospheric structure

5 104 K gas (EIT He 304 Å) 7000 K gas Ca II K

(11)

Chromospheric structure II

The chromosphere The chromosphere exhibits a very wide exhibits a very wide variety of structures.

variety of structures.

E.g., E.g.,

Sunspots and Sunspots and Plages

Plages

Network and Network and

internetwork (grains) internetwork (grains)

SpiculesSpicules

Prominences and Prominences and filaments

filaments

Flares and Flares and eruptions

eruptions

DOT G-band: photosphere DOT Ca II K core: chromosphere

(12)

Chromospheric structure

The chromosphere The chromosphere exhibits a very wide exhibits a very wide variety of structures.

variety of structures.

E.g., E.g.,

Sunspots and Sunspots and Plages

Plages

Network and Network and internetwork

internetwork

SpiculesSpicules

Prominences and Prominences and filaments

filaments

Flares and Flares and eruptions

eruptions

(13)

Chromospheric structure

The chromosphere The chromosphere exhibits a very wide exhibits a very wide variety of structures.

variety of structures.

E.g., E.g.,

Sunspots and Sunspots and Plages

Plages

Network and Network and internetwork

internetwork

SpiculesSpicules

Prominences Prominences and filaments and filaments

Flares and Flares and eruptions

eruptions

(14)

Chromospheric dynamics (DOT)

Network

Internetwork

(15)

Chromospheric dynamics

Oscillations, Oscillations, seen in

seen in cores of cores of

strong lines strong lines

Power at 3 Power at 3 min in Inter- min in Inter-

network network

Power at Power at 5-7 min in 5-7 min in

Network

Network

Lites et al. 2002

(16)

Models: the classical chromosphere

Classical picture: Classical picture:

plane parallel, plane parallel,

multi-component multi-component

atmospheres atmospheres

Chromosphere is Chromosphere is composed of a composed of a

gentle rise in gentle rise in temperature temperature

between

between TTminmin and and transition region.

transition region.

Fontenla et al. 1993

TTminmin

(17)

Need to heat the chromosphere

Radiative equilibrium, RE:Radiative equilibrium, RE:

only form of energy only form of energy

transport is radiation &

transport is radiation &

atmosphere is in thermal atmosphere is in thermal

equilibrium.

equilibrium.

VAL-C:VAL-C: empirical model empirical model

Dashed curves:Dashed curves: temp. temp.

stratifications for stratifications for

increasing amount of increasing amount of

heating (from bottom to heating (from bottom to

top).

top).

Mechanical heating Mechanical heating

needed to reproduce obs.

needed to reproduce obs. Anderson & Athay 1993Anderson & Athay 1993

(18)

Dynamic models

Start with piston in Start with piston in convection zone, convection zone,

consistent with obs. of consistent with obs. of

photospheric oscillations photospheric oscillations

Waves with periods of Waves with periods of

3min propagate into 3min propagate into chromosphere

chromosphere

Energy conservation Energy conservation

((ρρvv22/2 = const.) /2 = const.) & strong & strong ρ ρ decrease

decrease wave wave

amplitudes increase with amplitudes increase with

height: waves steepen height: waves steepen

and shock and shock

Temp. at chromospheric Temp. at chromospheric heights varies between heights varies between

3000 K and 10000 K

3000 K and 10000 K Carlsson & SteinCarlsson & Stein

(19)

Transition Region

Semi-empirical 1D-models of solar atmosphere: steep increase of T in transition region (TR): < 100 km thick

(20)

TR spatial structure

Lower transition Lower transition region (T<5 10

region (T<5 1055 K) K) shows structure very shows structure very

similar to similar to

chromosphere, with chromosphere, with

network, plage etc.

network, plage etc.

C IV (10C IV (1055 K) imaged K) imaged by SUMER

by SUMER

In upper transition In upper transition region structures are region structures are

more similar to corona more similar to corona

(21)

TR dynamic phenomena: blinkers

Brightness variability in the (quiet) transition region Brightness variability in the (quiet) transition region is larger than in any other layer of solar atmosphere is larger than in any other layer of solar atmosphere

Typical brightening: blinkersTypical brightening: blinkers

Occur everywhere, all the time. Last for minutes to Occur everywhere, all the time. Last for minutes to hours. How much of the brightening is due to

hours. How much of the brightening is due to overlapping overlapping

blinkers?

blinkers?

1 time step1 time step ≈ 1 minute≈ 1 minute

Si IV Si IV

(22)

Explosive events

Broadenings of TR spectral lines at 1-3 10Broadenings of TR spectral lines at 1-3 1055 K K

Typical “normal” line width 20 km/s, in explosive Typical “normal” line width 20 km/s, in explosive event: up to 400 km/s. Cover only a few 1000 km event: up to 400 km/s. Cover only a few 1000 km

and last only and last only

a few minutes a few minutes

Typically a Typically a few 1000

few 1000

present on

present on

Sun at any Sun at any

given time given time

(23)

The Solar Corona

Corona

Solar interior

Surface

While the surface While the surface

is about

is about 6,0006,000 KK, , the temperature in the temperature in

the corona the corona reaches about reaches about 2 2

million K.

million K.

What causes this What causes this rapid increase in rapid increase in temperature is still temperature is still

one of the big one of the big mysteries in solar mysteries in solar

physics.

physics.

(24)

The Hot and Dynamic Corona

EUV Corona: 106 K plasma (EIT/SOHO 195 Å)

White light corona

(LASCO C3 / SOHO, MPAe)

Corona at solar eclipse

(25)

Coronal structures

Active regions Active regions (loops)

(loops)

Quiet SunQuiet Sun

X-ray bright pointsX-ray bright points

Coronal holesCoronal holes

ArcadesArcades

Fe XII 195 Å

(1.500.000 K) 17 May - 8 June 1998

(26)

Coronal structure: active region loops

TRACE, 1999 TRACE, 1999

(27)

Coronal structure: streamers

(28)

The solar wind

A constant stream of particles flowing from the Sun’s A constant stream of particles flowing from the Sun’s

corona, with a temperature of about a million degrees corona, with a temperature of about a million degrees

and with a velocity of about

and with a velocity of about 450 km/s. The solar wind 450 km/s. The solar wind reaches out beyond Pluto's orbit, with the heliopause reaches out beyond Pluto's orbit, with the heliopause

located roughly at located roughly at

100-120 AU 100-120 AU

(29)

Comets and the solar wind

Comet NEAT (C/2002 V1)

(30)

Solar wind characteristics at 1AU

Fast solar wind Slow solar windFast solar wind Slow solar wind

speed > 400 km/s <400 km/sspeed > 400 km/s <400 km/s

nnpp 3 cm3 cm-3-3 8 cm 8 cm-3-3

homogeneous homogeneous high variabilityhigh variability

BB≈ 5 nT = 0.0005G B < 5 nT≈ 5 nT = 0.0005G B < 5 nT

95% H, 4% He95% H, 4% He94% H, 5% He94% H, 5% He

Alfvenic fluctuationsAlfvenic fluctuations Density fluctuationsDensity fluctuations

Origin: coronal holesOrigin: coronal holes Origin: in connection with coronal Origin: in connection with coronal streamers

streamers

Transient solar windTransient solar wind

speed from < 300 km/s up to >2000 km/sspeed from < 300 km/s up to >2000 km/s

Variable B, with B up to 100 nT (0.01G)Variable B, with B up to 100 nT (0.01G)

Often very low densityOften very low density

Sometimes up to 30% HeSometimes up to 30% He

Often associated with interplanetary shock waves Often associated with interplanetary shock waves

Origin: CMEsOrigin: CMEs

(31)

3-D structure of the Solar Wind:

Variation over the Solar Cycle

1st Orbit: 3/1992 - 11/1997

declining / minimum phase

2nd Orbit: 12/1997 - 2/2002

rising / maximum phase

Woch et al. GRL Ulysses SWICS data

(32)

Coronal Shape & Solar Wind:

Ulysses Data & 3D-Heliosphere

Activity minimum Activity maximum

Activity minimum Activity maximum

(33)

Parker’s theory of the solar wind

Basic idea: dynamic equilibrium between hot corona Basic idea: dynamic equilibrium between hot corona and interstellar medium. Mass and momentum

and interstellar medium. Mass and momentum balance equations:

balance equations:

Parker’s Eq. for solar wind speed (isothermal Parker’s Eq. for solar wind speed (isothermal atmosphere)

atmosphere)

2 2

1

0 )

(

r GM dr

dP dr

v dv

v dr r

d

2 2

2 2

2

) 1 (

r GM r

c c dr v

dv v

S

S

(34)

Parker’s solar wind solutions

Parker found 4 Parker found 4

families of solar wind families of solar wind

solutions solutions

2 not supported by 2 not supported by Obs. (supersonic at Obs. (supersonic at

solar surface) solar surface)

1 does not give 1 does not give

sufficient pressure sufficient pressure

against the against the

interstellar medium.

interstellar medium.

Correct solution must Correct solution must be thick line in Fig.

be thick line in Fig.

CHECK WHY ONLY ONE SOLN CHECK WHY ONLY ONE SOLN

IS CORRECT!!!!!!!!!

IS CORRECT!!!!!!!!!

(35)

Solar wind speed

Speed of Speed of solar wind solar wind

predicted by predicted by

Parker’s Parker’s

model for model for

different different

coronal coronal

temperatures temperatures

(simple, (simple,

isothermal isothermal

case; no case; no magnetic magnetic

field) field)

(36)

The Heliosphere

Heliosphere Heliosphere = region = region of space in which the of space in which the solar wind and solar solar wind and solar magnetic field

magnetic field

dominate over the dominate over the instellar medium and instellar medium and the galactic magnetic the galactic magnetic field.

field.

Bowshock:Bowshock: where the where the interstellar medium is interstellar medium is slowed relative to the slowed relative to the Sun.Sun.

Heliospheric shock: Heliospheric shock:

where the solar wind where the solar wind is decelerated relative is decelerated relative to Sun

to Sun

Heliopause:Heliopause: boundary boundary of the heliosphere

of the heliosphere Interstellar

Interstellar medium medium Bowshock

Bowshock

Heliospheric Heliospheric

shock shock Heliopause Heliopause

Heliotail Heliotail

(37)

Magnetic Field

(38)

  in order to in order to understand the understand the

dynamics and dynamics and activity of the

activity of the Sun Sun we need

we need

measurements and measurements and

theory of its theory of its magnetic field magnetic field

The source of the Sun’s The source of the Sun’s

activity is the magnetic field activity is the magnetic field

Thomas Wiegelmann Thomas Wiegelmann

(39)

Correlation of field with brightness

(40)

Open and closed magnetic flux Open and closed magnetic flux

Open flux: fast solar Open flux: fast solar

windwind

Closed flux: slow Closed flux: slow

solar wind solar wind

Most of the solar flux Most of the solar flux

returns to the solar returns to the solar

surface within a few surface within a few RR (closed flux) (closed flux)

A small part of the A small part of the

total flux through the total flux through the

solar surface solar surface

connects as open connects as open

flux to interplanetary flux to interplanetary

space space

(41)

Measured Magnetic

Field at Sun’s Surface

Month long Month long sequence of sequence of magnetograms magnetograms

(approx. one (approx. one solar rotation) solar rotation) MDI/SOHO MDI/SOHO

May 1998 May 1998

(42)

Methods of magnetic field measurement

Direct methods: Direct methods:

Zeeman effectZeeman effect  polarized radiation polarized radiation

Hanle effectHanle effect  polarized radiation polarized radiation

GyroresonanceGyroresonance  radio spectra radio spectra

Indirect methods: Proxies Indirect methods: Proxies

Bright or dark features in photosphere (sunspots, Bright or dark features in photosphere (sunspots, G-band bright points)

G-band bright points)

Ca II H and K plageCa II H and K plage

Fibrils seen in chromospheric lines, e.g. HFibrils seen in chromospheric lines, e.g. Hαα

Coronal loops seen in EUV or X-radiationCoronal loops seen in EUV or X-radiation

(43)

Example of proxies: Continuum vs. G- band

Continuum G-band Continuum G-band

(44)

Ca II K as a magnetic field proxy

Ca II H and K lines, Ca II H and K lines, the strongest lines the strongest lines in the visible solar in the visible solar spectrum, show a spectrum, show a

strongly increasing strongly increasing

brightness with brightness with

non-spot magnetic non-spot magnetic

flux.

flux.

The increase is The increase is slower than linear slower than linear

Magnetic regions Magnetic regions (except sunspots) (except sunspots)

appear bright in Ca appear bright in Ca

II: Ca plage and II: Ca plage and network regions network regions

(45)

Hα and the chromospheric field

HHαα images of active images of active regions show a

regions show a

structure similar to structure similar to iron filing around a iron filing around a

magnet. Do they magnet. Do they

(roughly) follow the (roughly) follow the

field lines?

field lines?

Relatively horizontal Relatively horizontal field in

field in

chromosphere?

chromosphere?

Note spiral structure Note spiral structure around sunspot.

around sunspot.

(46)

Zeeman diagnostics

Direct detection of magnetic field by Direct detection of magnetic field by

observation of magnetically induced splitting observation of magnetically induced splitting

and polarisation of spectral lines and polarisation of spectral lines

Important: Zeeman effect changes not just Important: Zeeman effect changes not just the spectral shape of a spectral line (often the spectral shape of a spectral line (often

subtle and difficult to measure), but also subtle and difficult to measure), but also

introduces a

introduces a unique unique polarisation signature polarisation signature



Measurement of polarization is central to Measurement of polarization is central to measuring solar magnetic fields.

measuring solar magnetic fields.

(47)

Polarized radiation

Polarized Polarized radiation is radiation is described bydescribed by the 4 the 4 StokesStokes

parameters: parameters: I, Q, UI, Q, U and and V V

I I = total intensity = total intensity == I Ilinlin(0(0oo) + ) + IIlinlin(90(90oo) =) = I Ilinlin(45(45oo) + ) + IIlinlin(135(135oo) = ) = IIcirccirc(right(right) +) + I Icirccirc(left) (left)

Q Q = = IIlinlin(0(0oo) - ) - IIlinlin(90(90oo) )

UU = = IIlinlin(45(45oo) - ) - IIlinlin(135(135oo) )

VV = = IIcirccirc(right) - (right) - IIcirccirc(left)(left)

Note: Stokes parameters are sums and differences of Note: Stokes parameters are sums and differences of intensities, i.e. they are directly measurable

intensities, i.e. they are directly measurable

(48)

Zeeman splitting of atomic levels

In the presence of a B-In the presence of a B- field a level with total field a level with total

angular moment J will angular moment J will

split into

split into 22J+1J+1 sublevels sublevels with different M.

with different M.

EEJ,MJ,M = E = EJJ++μμ0 0 gMgMJJBB

Transitions are allowed Transitions are allowed between levels with between levels with ∆J J

= 0,= 0,±1 & ±1 & M M = 0 (= 0 (ππ)), , ±1 ±1 ((σσbb, , σσrr))

Splitting is determined Splitting is determined by Lande factor

by Lande factor g g ::

gg((J,L,SJ,L,S) = 1+() = 1+(JJ((JJ+1)+ +1)+

SS(S(S+1)-+1)-LL(L(L+1))/2+1))/2J(J(J+1)J+1)

(49)

Splitting patterns of lines

Depending on g of the Depending on g of the upper and lower levels, upper and lower levels, the spectral line shows the spectral line shows

different splitting different splitting

patterns patterns

Positive: Positive: ππ components: components:

ΔΔMM=0=0

Negative: Negative: σσ components:

components: ΔΔMM=±1=±1

Top left: normal Top left: normal

Zeeman effect (rare) Zeeman effect (rare)

Rest: anomalous Rest: anomalous

Zeeman effect (usual) Zeeman effect (usual)

(50)

Polarization and Zeeman effect

(51)

Effect of changing field strength

Formula for Zeeman splitting (

Formula for Zeeman splitting (for for BB in G, in G, λλ in Å): in Å):

ΔλΔλHH = 4.67 10 = 4.67 10-13-13 ggeffeffBBλλ22 [Å] [Å]

ggeffeff=effective Lande factor of line=effective Lande factor of line For large

For large BB: : ΔλΔλHH = = ΔλΔλ between between σσ-component peaks-component peaks

B=200 G B=200 G B=1600 G

B=1600 G

I

V

(52)

Dependence on B, γ, & φ

I ~ I ~ κκσσ(1+(1+coscos22γγ)/4)/4 + + κκππ sin sin22γγ/2/2

Q ~ BQ ~ B22 sin sin22γ cos 2γ cos 2φφ

U ~ BU ~ B22 sin sin22γγ sin 2 sin 2φφ

V ~ BV ~ B cos cos γγ

Q, UQ, U: transverse: transverse component of component of BB

VV: longitudinal: longitudinal component of component of BB

Juanma Borrero Juanma Borrero

(53)

Zeeman polarimetry

Most used remote sensing of astrophysical Most used remote sensing of astrophysical (and certainly solar) magnetic fields

(and certainly solar) magnetic fields

Effective measurement of field strength if Effective measurement of field strength if Zeeman splitting is comparable to Doppler Zeeman splitting is comparable to Doppler

width or more:

width or more: B B > > 2 2 00 00 G … G … 1000 1000 G G (depending on spectral line)

(depending on spectral line)   works best in works best in photosphere

photosphere

Splitting scales with λ Splitting scales with λ   works best in IR works best in IR

Sensitive to cancellation of opposite magnetic Sensitive to cancellation of opposite magnetic polarities

polarities   needs high spatial resolution needs high spatial resolution

(54)

Fe I 630.2 nm

II VV

QQ UU

Fe I 1564.8 nm Fe I 1564.8 nm

Effect of wavelength of spectral line

(55)

Cancellation of magnetic polarity

Spatial resolution Spatial resolution

element element

= positive polarity

= positive polarity magnetic fieldmagnetic field

= negative polarity

= negative polarity magnetic fieldmagnetic field

(56)

Magnetograms

Magnetograph: Magnetograph:

Instrument that Instrument that

makes maps of (net makes maps of (net circular) polarization circular) polarization in wing of Zeeman in wing of Zeeman sensitive line.

sensitive line.

Example of Example of magnetogram magnetogram obtained by MDI obtained by MDI

Conversion of Conversion of polarization into polarization into magnetic field magnetic field

requires a careful requires a careful calibration.

calibration.

(57)

What does a

magnetogram show?

Plotted at left: Plotted at left:

Top:Top: Stokes Stokes I, QI, Q and and VV along along a spectrograph slit

a spectrograph slit

Middle:Middle: Sample Stokes Sample Stokes Q Q profile

profile

Bottom:Bottom: Sample Stokes Sample Stokes V V profile

profile

Red bars:Red bars: example of a example of a

spectral range used to make spectral range used to make a magnetogram. Generally a magnetogram. Generally only Stokes

only Stokes VV is used is used

(simplest to measure), gives (simplest to measure), gives longitudinal component of longitudinal component of BB..

(58)

Synoptic maps approximate the radial magnetic flux observed near the central meridian over a period of 27.27 days (= 1

Carrington rotation)

Synoptic charts

Synoptic charts

(59)

Polarized radiative transfer

Complication: RTE required for 4 Stokes Complication: RTE required for 4 Stokes

parameters: Written as differential equation for parameters: Written as differential equation for

Stokes vector

Stokes vector I I

νν

= = ( ( I I

ν ν

,Q ,Q

ν ν

,U ,U

ν ν

,V ,V

νν

) )

Eq. in plane parallel atmosphere for a spectral Eq. in plane parallel atmosphere for a spectral line (Unno-Rachkowsky equations):

line (Unno-Rachkowsky equations):

μ μ d d I I

ν ν

/ / d d τ τ

cc

= = Ω Ω

νν

I I

νν

– – S S

νν

Ω Ω

νν

= = absorption matrix (basically ratio of line to absorption matrix (basically ratio of line to continuum absorption coefficient),

continuum absorption coefficient), S S

νν

= = source source function vector,

function vector, τ τ

cc

= continuum optical depth. = continuum optical depth.

(60)

Polarized radiative transfer II

The absorption matrix The absorption matrix

SAY MORE ABOUT MATRIX ELEMENTS!!!!!!

SAY MORE ABOUT MATRIX ELEMENTS!!!!!!

SHOW HOW ZEEMAN EFFECT ENTERS SHOW HOW ZEEMAN EFFECT ENTERS

INTO THEM, ETC.!!!!!

INTO THEM, ETC.!!!!!

 

 

 

 

I Q

U V

Q I

V U

U V

I Q

V U

Q I

1 1

1

1

(61)

Polarized radiative transfer III

The Zeeman effect only enters through The Zeeman effect only enters through Ω Ω

νν

Ω Ω

νν

contains besides absorption due to contains besides absorption due to Zeeman-split line

Zeeman-split line ( ( η η

I I

, , η η

Q Q

, , η η

U U

, , η η

V V

) ) also also

magnetooptical effects, such as Faraday magnetooptical effects, such as Faraday

rotation

rotation ( ( ρ ρ

Q Q

, , ρ ρ

U U

, , ρ ρ

V V

) ) : rotation of plane of : rotation of plane of polarization when light passes through polarization when light passes through B. B.

Ω Ω

ν ν

= = Ω Ω

νν

( ( γ γ , , φ φ , B , B ) ) , i.e. , i.e. Ω Ω

νν

depends on the full depends on the full magnetic vector (in addition to the usual magnetic vector (in addition to the usual quantities that the absorption coefficient quantities that the absorption coefficient

depends on)

depends on)

(62)

LTE

In LTE the Unno-Rachkowsky equations simplify In LTE the Unno-Rachkowsky equations simplify since

since

SSνν= (= (BBν ν, , 0, 0, 0)0, 0, 0)

Here BHere Bν ν= Planck function= Planck function

Also,Also, ΩΩνν is simplified. The is simplified. The ηηI I , , ηηQ Q , , ηηU U , , ηηV V and and ρρQ Q , , ρρU U , , ρρV V values only require application of Saha- values only require application of Saha-

Boltzmann equations (similar situation as for LTE in Boltzmann equations (similar situation as for LTE in

case of normal radiative transfer). Each of these case of normal radiative transfer). Each of these

quantities is, of course, frequency dependent.

quantities is, of course, frequency dependent.

(63)

Solution of Unno Eqs

General solution best done numerically (even formal General solution best done numerically (even formal solution is non-trivial: exponent of matrix

solution is non-trivial: exponent of matrix ΩΩνν))

Simple analytical solutions exist for a Milne-Simple analytical solutions exist for a Milne- Eddington atmosphere (i.e. for

Eddington atmosphere (i.e. for ΩΩνν independent of independent of ττνν and and SSνν depending only linearly on depending only linearly on ττνν). ). Particularly Particularly

simple if we neglect magneto-optical effects simple if we neglect magneto-optical effects

I(I(μμ) = ) = ββ μμ (1+ (1+ηηII)/)/ΔΔ

P(P(μμ)= )= ββ μμ ηηPP//ΔΔ,, wherewhere P = Q, U,P = Q, U, oror VV

ΔΔ = (1+ = (1+ηηII))2 2 --ηηQQ2 2 --ηηUU2 2 --ηηVV2 2 takes care of line saturationtakes care of line saturation

ββ is derivative of Planck function with respect tois derivative of Planck function with respect to ττνν . .

(64)

Basics: magnetic pressure

Magnetic field exerts a pressure. Pressure balance between Magnetic field exerts a pressure. Pressure balance between two components of the atmosphere, 1 and 2 (Gauss units):

two components of the atmosphere, 1 and 2 (Gauss units):

If, e.g. If, e.g. BB2 2 = 0, = 0, then then PP11 < < PP22 and it follows: and it follows:

Magnetic features are evacuated compared to surroundings.Magnetic features are evacuated compared to surroundings.

If If BB2 2 = 0= 0 and and TT11 = T = T22, then also , then also ρρ11 < < ρρ22 , so that the magnetic , so that the magnetic features are buoyant compared to the surrounding gas.

features are buoyant compared to the surrounding gas.

In the convection zone this buoyancy means that rising field In the convection zone this buoyancy means that rising field bundles (flux tubes) keep rising (unless stopped by other

bundles (flux tubes) keep rising (unless stopped by other forces, e.g. curvature forces.

forces, e.g. curvature forces.

 8

8

2 2 2

1 2

1

B

P

BP  

(65)

Basics: plasma β

Plasma Plasma ββ describes the ratio of thermal to magnetic describes the ratio of thermal to magnetic energy density:

energy density:

ββ < 1< 1  Magnetic field dominates and dictates the Magnetic field dominates and dictates the dynamics of the gas

dynamics of the gas

ββ >1>1  Thermal energy, i.e. gas dominates & forces Thermal energy, i.e. gas dominates & forces the field to follow

the field to follow

ββ changes with changes with r/Rr/R

β β >1 >1 in convection zonein convection zone

β <β <1 1 in atmosphere, particularly in corona in atmosphere, particularly in corona ββ <<1 <<1

2

8 B

P

 

(66)

Supergranules and magnetic field

Magnetogram:Magnetogram: black and black and white patches

white patches

Horizontal velocity:Horizontal velocity:

arrows arrows

Divergence:Divergence:

blue arrows > 0;

blue arrows > 0;

red arrows: < 0 red arrows: < 0

Supergranule boundaries:Supergranule boundaries:

yellow yellow

Magnetic field is Magnetic field is

concentrated at edges of concentrated at edges of

supergranules supergranules

B swept out by flowB swept out by flow

(67)

Frozen-in magnetic fields

Magnetic field is swept to supergranule boundaries Magnetic field is swept to supergranule boundaries

 magnetic field is “frozen” into the plasma magnetic field is “frozen” into the plasma

This happens if there are a sufficient number of This happens if there are a sufficient number of ionised particles, or equivalently, if the electric ionised particles, or equivalently, if the electric

conductivity is very high, since charged particles conductivity is very high, since charged particles

cannot cross field lines (gyration) cannot cross field lines (gyration)

This is the case, even in the cool photosphere of This is the case, even in the cool photosphere of sunspots (only 10

sunspots (only 10-4-4 of all particles are ionized), due of all particles are ionized), due to the large number of collisions

to the large number of collisions

If plasma moves perpendicularly to the field, it drags If plasma moves perpendicularly to the field, it drags the field with it (or is stopped by the field) and vice the field with it (or is stopped by the field) and vice

versa. Flows parallel to the field are unaffected.

versa. Flows parallel to the field are unaffected.

(68)

Emergence of a magnetic flux tube

Magnetic field is believed to be generated mainly in the Magnetic field is believed to be generated mainly in the

Tachocline near bottom of convection zone.

Tachocline near bottom of convection zone.

Due to its buoyancy (see earlier slide; Parker instability), a Due to its buoyancy (see earlier slide; Parker instability), a magnetic field will rise towards the solar surface. At the solar magnetic field will rise towards the solar surface. At the solar

surface it will produce a bipolar active region.

surface it will produce a bipolar active region.

(69)

Emergence and evolution of active

region: GET BETTER MOVIE!!!!!!!!!!

(70)

The photospheric field

Sunspot Sunspot

umbra umbra

penumbra penumbra

plage plage quiet

quiet SunSun

(71)

Sunspots

Umbra Umbra Penumbra Penumbra Granule Granule

T T

eff eff

4500 K 4500 K

T T

eff eff

≈ 5500 K ≈ 5500 K

T T

eff eff

≈ 5800 K ≈ 5800 K

(72)

Sunspots, some properties

Field strengthField strength: Peak values : Peak values 2000-3500 G

2000-3500 G

BrightnessBrightness: umbra: 20% of : umbra: 20% of quiet Sun, penumbra: 75%

quiet Sun, penumbra: 75%

SizesSizes: Log-normal size : Log-normal size distribution. Overlap with distribution. Overlap with

pores (log-normal = pores (log-normal =

Gaussian on a logarithmic Gaussian on a logarithmic

scale) scale)

LifetimesLifetimes: : T T between hours & between hours &

months: Gnevyshev- months: Gnevyshev-

Waldmeier rule:

Waldmeier rule: AAmaxmax ~ ~ T, T, where

where A Amax max = max spot area.= max spot area.

(73)

Why are sunspots dark?

Basically the strong nearlly vertical magnetic field, not Basically the strong nearlly vertical magnetic field, not

allowing motions across the field lines, quenches convection allowing motions across the field lines, quenches convection

inside the spot.

inside the spot.

Since convection is the main source of energy transport just Since convection is the main source of energy transport just below the surface, less energy reaches the surface through below the surface, less energy reaches the surface through

the spot

the spot dark dark

(74)

Why are sunspots dark? II

Where does the energy blocked by sunspots go?Where does the energy blocked by sunspots go?

Spruit (1982) showed: both heat capacity and Spruit (1982) showed: both heat capacity and thermal conductivity of CZ gas is very large

thermal conductivity of CZ gas is very large

High thermal conductivity: blocked heat is High thermal conductivity: blocked heat is

redistributed throughout CZ (no bright rings around redistributed throughout CZ (no bright rings around

sunspots) sunspots)

High heat capacity: the additional heat does not lead High heat capacity: the additional heat does not lead to a measurable increase in temperature

to a measurable increase in temperature

In addition: time scale for thermal relaxation of the In addition: time scale for thermal relaxation of the CZ is long, 10

CZ is long, 1055 years: excess energy is released years: excess energy is released almost imperceptibly.

almost imperceptibly.

(75)

Magnetic structure of sunspots

Peak field strength Peak field strength ≈ 2000 – ≈ 2000 – 3500 G (usually in darkest, 3500 G (usually in darkest,

central part of umbra) central part of umbra)

B drops steadily towards B drops steadily towards boundary,

boundary, BB((RRspotspot) ≈ 1000 G) ≈ 1000 G

At centre, field is vertical, At centre, field is vertical, becoming almost horizontal becoming almost horizontal

near

near RRspotspot . .

Regular spots have a field Regular spots have a field structure similar to a buried structure similar to a buried

dipole dipole

(76)

Magnetic structure of

sunspots II

Azimuthal averages of Azimuthal averages of

the various magnetic the various magnetic field components in a field components in a sample of regular (near- sample of regular (near- circular) medium-sized circular) medium-sized

sunspots.

sunspots.

(77)

Magnetic structure of sunspots

Regular on large scales (Regular on large scales (≈ dipole, B dipole, Bmaxmax ≈ 2500 G, ≈ 2500 G, for simple for simple spots)

spots)

Extremely complex on small scales (penumbra, subsurface)Extremely complex on small scales (penumbra, subsurface)

Schlichenmaier et al.

1998, 1999, 2002

(78)

Sunspot fine structure

Penumbral filaments Penumbral filaments

(bright and dark) (bright and dark)

Penumbral grain (seen Penumbral grain (seen

to move inward) to move inward)

Light bridge Light bridge

Umbral dot Umbral dot

(79)

Highest resolution

Scharmer et al. 2002 Scharmer et al. 2002

(80)

Sunspots

TiO Zakharov 2004

(81)

Umbral dots seen in TiO

V. Zakharov

(82)

Magnetic structure of sunspots

Sunspots span too many spatial and temporal scales Sunspots span too many spatial and temporal scales

to be successfully simulated from first principles.

to be successfully simulated from first principles.

X ?

References

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