Download - Sun Planet Connection Lecture 2013 | MPS
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Sun-planet connection
Chap. 1 Plasma
Chap. 2 Sun
Chap. 3 Earth
Chap. 4 Planets
IMPRS Solar System School Retreat, Apr 29 – May 2, 2013
Y. NaritaSpace Research Institute
Austrian Academy of Sciences
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Ionization of atomic hydrogen gas
Other ionization sources?
13.6 eV = 158 000 K
H → p + e-
1AU corona
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Magnetohydrodynamics
Flow velocity evolution
Simplified pressure balance
Magnetic field evolution
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Pressure balance realizations
(a) Hydrostatic equilibrium
(c ) Rotating body (d) Radiative transfer
pmagpdyn
Φgrav
pth
(b) Hydromagnetic equilibrium
ΦgravΦgrav
prad
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Energy conversion processes
Ekin
reconnection
shock wave
dynamoT-tauri stars
solar wind
Eth
Emag
Erad
Egrv
Eddinton luminosity
waves andturbulence
cooling
contraction
heating
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Heat energy transport
Caveat! Additional energy loss due to neurtino escape
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Exercise
Is the electrical conductivity in interplanetary plasma (at 1 AU)better than that of iron Fe (107 Ω-1 m-1)?
How many meaningful units are there for expressing pressure?
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Solution
Is the electrical conductivity in interplanetary plasma (at 1 AU)better than that of iron Fe (107 Ω-1 m-1)?
How many meaningful units are there for expressing pressure?
The resistivity formula (η=σ -1 = me νc / ne e2 ) using ne= 10 cm -3
and νc = 10-7 Hz (Te = 0.3 MK) yields σ = 106 Ω-1 m-1. It is less conductive than iron but is almost on the same order.
Pa (pascal)N/m2 (force per area)J/m3 (energy density)kg ms-1 / m2 s (momentum flux)
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Heat production
Chap. 2 Sun
neutrinos
from gravitational contraction
from nuclear fusion
Reaction process
(pp-chain, CNO-cycle)
Is the core hot enough for fusion? … Yes but only possible through tunnel effect
Solar luminosity
heat
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Heat transfer to the surface
Core Radiative transport Convective transport Corona
Tachocline Chromosphere
FradFcnv
6000K
Surface
Model construction ● Spherical symmetry● Hydrostatic equilibrium● Equation of state?
Eth → Ekin →Emag
1 MK15 MK
ν
Lⵙ
Energy conversion
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Excursion to astrophysicsMain sequence stars
Low-mass (M)red dwarf, 0.1-0.5 Mⵙ
Sun-like (G)0.5-1.5 Mⵙ
High-mass (O,B)1.5 Mⵙ or higher
High-mass stars live much shorter although they have more fuel. Why?
core - conv
core - rad - conv
core+conv - rad
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Convection zone
Twisting magnetic field lines (“alpha”)
Stretching field lines (“Omega”)
Differential rotation
Cause of 11-year (or 22-year) perioditicy?
Buoyancy + Coriolis effect
Rad
Cnv
Taylor column
v
B
vB
fast
slow
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Corona
Proposed heating mechanisms: shock waves, nanoflares, Alfven waves, ...
Slice along the rot axis
Thermal expansion of coronal gas → solar wind (Eth → Ekin)
Slice cutting the rot axis
Vsw = cs
10Rⵙ
Thomson scattering
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Heliosphere
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Exercise
2. Is the number density of solar neutrino coming to Earth higher than 1 cm-3?
1. Estimate the lifetime of the sun.
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Solution
1. Estimate the lifetime of the sun.
(Fuel amount) = (Mⵙ / mp) [protons] x 26/4 [MeV] x 1.6 x 10-13 [J/MeV](Consumption rate) = Lⵙ = 4 x 1026 [J/s](Lifetime) = (Fuel) / (Consumption) = 2.9 x 1018 [s] = 0.9 x 1011 [yr]
Use solar constant and reaction rate (2 neutrinos per 26 MeV).Neutrino number flux is F = 1.36 x 103 [J/m2s] / (13 [MeV] x 1.6 x 10-13 [J/MeV]) = 6.5 x 1010 [particles / cm2s]Number density (on using the light speed c) is n = F/c = 2.18 x 106 [particles m-3] = 2.18 [particles cm-3].
It is slightly more than one particle per cm3.
2. Is the number density of solar neutrino coming to Earth higher than 1 cm-3?
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Earth's magnetic field boundary
Chap. 3 Earth
Time scale of reaction against solar wind change?
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Magnetosphere
Equlibrium picture
● How does the tail form? - Friction model vs. reconnection model● Where is the pressure balance applicable? And what kind of pressure?
Solar wind plasma
10 RE
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Magnetic field transport
Reconnection model (Dungey, 1961)
Friction model (Axford & Hines, 1961)
B
vv with shear
B
B reconnected
v
Bsun
Bearth
v
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Magnetospheric dynamics
Phenomenon with the southward directionof interplanetary magnetic field
compression
Geomagnetic storm Auroral substorm
reconnection
jet
Phenomenon with sudden increaseof solar wind pressure (CME, CIR)
Dayside compression ~ minutes
Nightside compression ~ hours
Recovery ~ days
Dayside reconnection ~ minutes
Tail reconnection ~ 40 minutes after dayside reconnection
Recovery ~ hours
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Exercise
Earth climate …
1. What can be used as a proxy of past Earth climate and solar activity on the timescale from 1000 to 10,000 years?
2. Draw footprint motion of Earth's magnetic field line in the arctic region.
Friction model Reconnection model
0h
6h18h
12h
Solar activity …
0h
6h18h
12h
viewed from north pole axis to the ionosphere
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Solution
Earth climate … Oxygen 18 isotope abundance in stalagmite
1. What can be used as a proxy of past Earth climate and solar activity on the timescale from 1000 to 10,000 years?
2. Draw footprint motion of Earth's magnetic field line in the arctic region.
Friction model Reconnection model
0h
6h18h
12h
Solar activity … Carbon 14 isotope abundance in tree ring
0h
6h18h
12h
viewed from north pole axis to the ionosphere
(Neff et al., Nature, 411, 290, 2001)
dayside reconnection
tail reconnection
friction at flank of magnetopause
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Obstacle types
Chap. 4 Planets
Magnetized body Umagnetized body
Without atmosphere
With atmosphere Earth
Gas giants (J, S)
Icy planets (U, N)
Mercury
Venus, Mars
Earth moon
Ganymede
Titan, Enceladus
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Dipole axis and magnetosphere size
Merc Earth
J, S U, N
2 Rpl 10 Rpl
70 Rpl (J), 20 Rpl (S) 25 Rpl
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Rocky planetsMercury
2 Rpl
Venus
Earth
Mars1%-10% Rpl
10 Rpl
1%-10% Rpl
Induced magnetosphere
Substorm, aurora
No inosophere but substorm-like events
Crustal magnetic field
No planetarymagnetic field
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Gas giants (Jup,Sat)
Centrifugal force
10-hour rotation
Liquid, metalic hydrogen envelope?
Satellites as plasma source (Io, Enceladus)
Aurora, radio wave, synchrotron emission
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Icy planets (Ura, Nep)
Planet formation beyond ice limit
Large tilt angle → pole-on magnetosphere
Aurora, radio wave emission
pole-on pole-off
solar wind solar wind