Lecture 16 - The solar surface and atmosphere o Topics to be covered: o Photosphere o Chromosphere o Transition region o Corona The solar atmosphere o Photosphere o T ~ 5,800 K o d ~ 100 km o Chromosphere o T ~ 105 K o d <2000 km. o Transition Region o T ~ 105.5 K o d ~2500 km o Corona o T >106 K o d >10,000 km The photosphere o T ~ 5,800 K o r ~ RSun o Photosphere is the visible surface of the Sun. o At the photosphere, the density drops off abruptly, and gas becomes less opaque. o Energy can again be transported via radiation. Photons can escape from Sun. o Photosphere contains many features: o Sunspots o Granules β= PG 2nkT = 2 PB B /8π >>1 in photosphere € The photosphere (cont.) o Sunspots are dark areas in the photosphere. o F o r m e d b y t h e concentration of large magnetic fields (B>1000 G). o Sunspots appear dark because they are cooler (~4,300 K). o Granulation is a small scale pattern of convective cells o R e s u l t s f r o m temperature gradients close to the solar surface. Determining the photospheric temperature. o The Sun emits a blackbody spectrum with peak 2.8978 × 10−3 T= λ peak o Using Wein’s Law: K and λ peak = 5100 × 10 −10 m € € Tsun 2.8978 × 10 −3 = 5100 × 10 −10 ~ 5700 K peak ~ 5100 Å The solar constant o We know from Stephan-Boltzman Law that L=A T4 W o A is area of Sun’s surface, T is temperature, and (5.67 10-8 W m-2 K-4). is Stephan-Boltzman constant o The flux reaching the Earth is therefore: F = L / 4πd2 = 4πR2 T4 / 4πd2 Wm-2 [d = 1AU, R = solar radius] = T4 (R/d)2 = 1396 W m-2 o This is relatively close to the measured value of 1366 W m-2. The solar constant o The “solar constant” actually has a tiny variation (~0.1%) with the solar cycle. o Represents the driver for Earth and planet climate modelling. The chromosphere o Above the photosphere is a layer of less dense but higher temperature gases called the chromosphere. o First observed at the edge of the Moon during solar eclipses. o Characterised by “spicules”, “plage”, “filaments”, etc. o Spicules extend upward from the photosphere into the chromosphere. The chromosphere (cont.) o Prominence and filaments are cool volumes of gas suspended above the chromosphere by magnetic fields. o Plage is hot plasma (relative to the chromosphere), usually located near sunspots. Model solar atmosphere β >> 1 € β << 1 € β ~ 1? € β= € PG PB The corona o Hot (T >1MK), low density plasma (i.e. an ionized gas). o There are currently two coronal heating theories: o Magnetic waves (AC). o Magnetic reconnection (DC). o Coronal dynamics and properties are dominated by the solar magnetic field. β= € PG 2nkT = 2 << 1 PB B /8π Yohkoh X-ray image Static model of the corona o Assuming hydrostatic equilibrium: dP = −gρ dr Eqn. 3 where the plasma density is =n (me+mp) ≈ nmp (mp= proton mass) and both electrons and protons contribute € to pressure: P = 2 nkT = 2 kT/mp o Substituting into Eqn.3, and integrating => where 2kT dρ = −gρ m p dr $ mgr ' ρ = ρ 0 exp&− ) % kT ( € 0 is the density at r ~ R. The scale height is H = kT / mg. € o OK in low coronae of Sun and solar-type stars (and planetary atmospheres). Static model of the corona o Chapman (1957) attempted to model a static corona with thermal conduction. o Coronal heat flux is q= where thermal conductivity is o In absence of heat sources/sinks, T = 0T 5/2, q = 0 => ( 0T 5/2 T) = 0 o In spherical polar coordinates, 1 d# 2 5 / 2 dT & r κ T % (=0 0 r 2 dr $ dr ' € Eqn. 1 Static model of the corona r 2κ 0T 5 / 2 dT =C dr o Eqn. 1 => o Separating variables and integrating: € o 5/2 dT = C κ0 dr ∫r 2 2 C1 => T 7 / 2 = − 7 κ0 r To ensure T = T0 at r = r0 and T ~ € 0 as r € o ∫T ∞ set # r0 & 2 / 7 ∴T = T0 % ( $r' € r0T07 / 2 = − C 7 κ0 2 Eqn. 2 For T = 2 x 106 K at base of corona, ro = 1.05 R => T ~ 4 x 105 K at Earth (1AU = 214R). Close to measured value. € Static model of the corona o Subing for T from Eqn. 2, and inserting for P into Eqn. 3 (i.e., including conduction), 2/7& # #r & d ρ kT0 % 0 ( %%2 $r' dr $ m p GMm p ρ 1 dρ ρ − 2 /7 = − r 2 / 7 dr r9/7 2kT0 r02 / 7 r 2 o Using multiplication rule, € ∫ € GMρ (( = − 2 r ' GMm p r dr dρ = 2 /7 − ∫ ρ0 ρ r0 r 2kT0 r02 / 7 ρ ∫ dr r0 r12 / 7 r 7 GMm p r05 / 7 ln( ρ / ρ 0 ) = 2 /7ln(r /r0 ) + 5 2kT0 r0 r 5 / 7 € # 7 GMm *# r & 5 / 7 -& # r &2 / 7 p ρ(r) = ρ 0 % ( exp%% ,% 0 ( −1/(( $ r0 ' .' $ 5 2kT0 r0 +$ r ' € € Eqn. 4 Static model of the corona o Both electrons and protons contribute to pressure: P = 2 nkT = 2 o Substituting into Eqn. 4 => o As r ∞, Eqn.4 => " 7 GMm )" r % 5 / 7 ,% p P(r) = P0 exp$$ +$ 0 ' −1.'' -& # 5 2kT0 r0 *# r & € ∞ and Eqn. 5 => P const >> PISM. o PISM ~ 10-15 P0. Eqn. 5 => P ~ 10-4 P0 => There must be something wrong with the static model. kT/mp Eqn. 5
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