Doctorate Thesis DEMETER Satellite Data Analysis of Seismo ...

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p ∇ ·i = 0 ∇[σ(∇Φ + C∇p)] = 0 σij E σik = ∂ F δik + F ∂uik F uik δik T,E d F = −SdT + σikduik − 1 4π D · d E T S D Ψ = F − uikσik d Ψ = −SdT + uikdσik − 1 4π D · d E ∂ uik = − Ψ ∂σik T,E
Ψ σik E uik = µiklmσlm + γl,ikEl γl,ik µiklm M UME UME = −aiklmσikmlmm aiklm m M ΨP M = −λi,klHiσkl
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· ·
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· ·
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∼
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∼
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∼
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∼
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s 1/2
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∆wσ hcumratio
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∆wσ hcumratio
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σ
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∆wσ
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∆wσ abs(∆latmag) ∆t
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{L, αIDP } 1.7 < L <
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RP M
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RP M
Page 36 and 37: Ψ i Ψ e Ψ( R) Ψ i =
Page 38 and 39: Sq SD
Page 40 and 41: ≈ ÷ ≈ ÷
Page 42 and 43: J1 µ ω
Page 44 and 45: f0 α
Page 46 and 47: H = kT/mg z
Page 48 and 49: j j = σ // E// + σp
Page 50 and 51: sub−sections
Page 52 and 53: df/dt > 0 f < fH fH
Page 54 and 55: 70 o 50 o 30 o
Page 56 and 57: σ0
Page 58 and 59: ENR ET EF
Page 60 and 61: ≤ > 3.0 1
Page 62 and 63: 10 3 − 10 4
Page 64 and 65: vP /vS
Page 66 and 67: T = 10 0.5M−2.1 yr
Page 68 and 69: • • • •
Page 70 and 71: • • • •
Page 72 and 73: ∼ ÷
Page 74 and 75: σ
Page 76 and 77: ÷
Page 78 and 79: ÷ ÷ ∼
Page 80 and 81: ∆T = TEQ − TP B TEQ
Page 82 and 83: ∆T = TEQ − TP B TEQ
Page 84 and 85: ζ
Page 88 and 89: λi,kl
Page 90 and 91: ∇ ∧ js = 0 js
Page 92 and 93: x tk Ri xi
Page 94 and 95: e −(πωµσ)1/2 z z ω
Page 96 and 97: z = 0 z0 = 30 z = 50
Page 98 and 99: ≈ ÷
Page 100 and 101: ≈ ÷
Page 102 and 103: ≈ ÷
Page 104 and 105: ′
Page 106 and 107: • •
Page 108 and 109: • • •
Page 110 and 111: s 1 2 Do f < 2
Page 112 and 113: D(s 1 2 ) 1 2 3 4 5
Page 114 and 115: D(s 1 2 ) 1 2 3 4 5
Page 116 and 117: 5759 − 1
Page 118 and 119: ±16 ◦
Page 120 and 121: NP EAK NINC
Page 122 and 123: NP EAK NINC
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Page 130 and 131: − −− (1/128)s −1
Page 132 and 133: Latitude (deg) Latitude (deg) Latit
Page 134 and 135: Latitude (deg) Latitude (deg) Latit
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Latitude (deg) 90 45 0 -45 -90 DUR
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∆wσ hcumratio
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× 2 th
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±2 o
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∆t (TD − TEQ)
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∆wσ
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geocentric lat (deg) geocentric lat
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∆wσ hcumratio
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∆latmag∆t ∆latmag > 0
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∆wσ hcumratio ∆latmag ∆t
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(Delta magn lat) (deg) (Delta magn
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∆t ∆latmag
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∆latmag ∆wσ hcumratio
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CPhDemeter-λm EQ) (λ m D -λ m EQ
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∆wσ hcumratio
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∆T ∼ 4 ÷ 5
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mm 2 (Φ = 25mm)
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geocentric lat (deg) 50 0 -50 L she
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L L L L 10 8 6 4 2 0 10 8 6 4 2 0 1
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Latitude (deg) Latitude (deg) Latit
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{L, αIDP } 1.7 < L <
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1200 km ∆T
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∆T • •
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∆T • •
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H +
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f = 1 ± 0, 5kHz) f = 4, 5 ±
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(L/2) −4 cm −3
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F = J p 2 (cm 2 s sr
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Eres−rel = −δ − δ 2 − 4
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Eres−rel = −δ − δ 2 − 4
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Eres−rel = −δ − δ 2 − 4
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c = 2.99 × 10 8 [m/s] m = 9.1 × 1
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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Energy(KeV) 10 5 10 4 10 3 10 2 10
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BZ
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BZ
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BZ
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BZ
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BZ
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BZ
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Doctorate Thesis DEMETER Satellite Data Analysis of Seismo ...

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