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INVERSION OF SYNTHETIC APERTUR,E R,
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ñr^-- ltoN. J00NG suN '¿i¡r"r os
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I heleby declale that I am tlie sol
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plot of the maximum amplitude of th
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Contents Abstract Acknowledgements
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6.3.1 Introduction ..151 6.3.2 Digi
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5.1 Florv chart fot the proposecl i
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List of Tables 2,1 Seasat SAR senso
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List of Notations cr squint angle P
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tist of Abbreviatíons SAR Syntheti
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The objectives of this thesis rnay
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Ground Range l;l 2 sin0 Figure 1.2:
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ol'cler to evaluate its full aclvan
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algolithrn extlacts the complex bac
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successful as expected. Thele ale,
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eú ø1. [103]). Similal clevelopme
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aerial plìotogl'aphy ovel the area
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2.2 Spaceborne SAR Systems 1) SEASA
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tlie basis of a distinctive dlainag
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set fol selectecl aleas, useful for
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3) ERS-I The first European rernote
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Table 2.4: ERS-I Ðieterle [104]).
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Table 2.6: ERS-1 SAR pelfolmance re
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Table 2.7: JtrRS-1 olbit pararnetel
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Table 2.9: Chalactelistics of OPS o
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Table 2.11: Specifications of Racla
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Chapten 3 Review of Digital SAR Pro
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,I Figule 3.1: Raclar' L¡earn geom
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I L-=J}"no Figure 3.2: Geouretry fo
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vhich is the clistance across the a
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vlrere ø6 is a angular center fi'e
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à1 äl (a) /1T. or^l - r+ (b) I à
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a,pploxirnated by l2p sinl(I - ltl)
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-s(cu) is rewlitten as s@¡ - !"-,r
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cliscussecl later il this sectio¡r
- Page 71 and 72: Ïon = _2 (V(ro) .V(¿o)+ R(ro) .A(
- Page 73 and 74: : Range Walk : Range Curvatule : Ra
- Page 75 and 76: olbital SAR is given by Ion = -'#{t
- Page 77 and 78: is constant cluling the receiving p
- Page 79 and 80: a at f¡r
- Page 81 and 82: 'rvith a foulula developed il this
- Page 83 and 84: Chapter 4 Theoretical Development 4
- Page 85 and 86: developed and cliscussed by several
- Page 87 and 88: vhere u (r,ro; u) : I U 1r,ro,t)e-i
- Page 89 and 90: wheÌe k':frf a¡cl lc -_ uf us ant
- Page 91 and 92: 4) there is relative motion of ante
- Page 93 and 94: o =løo, 0, 0) Figure 4.1: Schemati
- Page 95 and 96: elorv that sulface. In genetal, sul
- Page 97 and 98: 4.4 The Inversion The equation Eq.(
- Page 99 and 100: *'here % is a platfolrn velocity an
- Page 101 and 102: The trq.(a.36) cannot be used dilec
- Page 103 and 104: vhele Àl is a tvavenurnbel collesp
- Page 105 and 106: 2-D FFT o(,b,;ø) Intelpolation in
- Page 107 and 108: ¡nE 0$r-sEc, ¡3 I IrlÊ [18- 5EC
- Page 109 and 110: 5.2 Digital Simulation Digital sirn
- Page 111 and 112: Table 5.2: Moclel palametels fol di
- Page 113 and 114: signal and the leconstructe
- Page 115 and 116: (3 È. e tc o) o -tl a Slant Range
- Page 117 and 118: that the inversiol method can accor
- Page 119 and 120: (n t0 Ê) 0c (lr) Figure 5.6: Seasa
- Page 121: 5.3 Processing of Real SAR Data A s
- Page 125 and 126: Aziurutì (n Þ !d !D gc Figule 5.1
- Page 127 and 128: (n 5 F Þ tq Figu.e 5.11: Reconst.u
- Page 129 and 130: over tlìe 2.4 inches as shol¡l i'
- Page 131 and 132: Ø Þ :J m (a) (b) ^a ctl _= a"r ro
- Page 133 and 134: Chapter 6 SAR fmage Enhancement for
- Page 135 and 136: 1) hoiv can the tlends of lineament
- Page 137 and 138: 6.2 Determination of Geological Str
- Page 139 and 140: Coolclinates for the image space an
- Page 141 and 142: Figure 6.2: Point, lines, and hyper
- Page 143 and 144: scatteter (e.g. coller leflectols,
- Page 145 and 146: Figure 6.5: CCRS's airboure C-band
- Page 147 and 148: C-l¡ancl SAR irnagery ovel this al
- Page 149 and 150: Figure 6.8: Radon transform of ailb
- Page 151 and 152: in the irnage space ancl the Iine i
- Page 153 and 154: ERS- 1 N U 0 rl 0o |lO + ,¡l r.l p
- Page 156 and 157: 6.2,3 Correlation Using The Radon T
- Page 158 and 159: Since the inside of the squale blac
- Page 160 and 161: Figule 6.12: Model test for correla
- Page 162 and 163: thlough the Radon tlansfolm is shor
- Page 164 and 165: Figure 6.15: Airborne C-band SAR da
- Page 166 and 167: distinct points can be cliscelnerl
- Page 168 and 169: Figure 6.18: Correlation output thr
- Page 170 and 171: 6.3 Merging of Multiple SAR Image D
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in Figure 6.19 tvhich is a clilect
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Figure 6.20: Additive irnages rvith
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Figule 6.22: Subtractive images rvi
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(1) select a clirection to be enhan
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Figure 6.24: Lnage obtained through
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6.3.4 Principal Components Analysis
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Table 6.2: Con'elation coeffrcielt
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Figure 6.27: The PCA frrst componen
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the geological surface lilearrent f
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ackscatte.i'g coefficiert can be cl
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Appendices A. Derivation of Forward
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B. Derivation of Inversion Formula
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C. Derivation using the Method of S
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F[eferences [1] Ahmed, S., \Vallen,
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[20] Curlis, J.D,, Flost, V.S., Del
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[43] Holn, R., 1988, E-SAR - The ex
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[65] Lotrelrl, O., 1990, Dopplel ce
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[87] Pye, 8.G., Nalch'ett,4.J., anc
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[111] \,Vu, C., Balkan,8., I(arplus