[99] Stolt, R.H., 1978, Migr.ation by Four.iel transfolrn, Geophysics, v.4J,, pp.23-48. [i00] Torniyasu, I{., 1978, Tutorial leview of synthetic ape-,-tule r.adar' (<strong>SAR</strong>) with applications to imaging of the ocean sutfaco, Proc. IEEE, v .66, no.5, pp.563-583. f101] Trevett, J.W., 1986, Imagnt.g Radar for Resource ,9urueys,, Chaprnan ancl Hall. [102] Ulaby, F.T., Moore, R.l(., and Fung, A,I(., 7g87, Microuaue Re¡note ,Sensing, Actiue a¡¿d Passiue: Vol.1, Aclclison-Wesley. [103] Ulaby, F.T., Moore, R.I(., ancl Furg, A.I(., 1982, Microwaue Retnote ,9ettsing, Actiae and Passiae: Vo1.2, Adclison-Wesley. [104] Velten, E.H. ancl Dietelle, G.H., 1986, Developrnent status of the ERS-1 payloacl instrurnents, Proc. I G A RS S' 8 6, Ztticlt, pp. 1 61- 1 66. [t05] Wang, J., Howalth, P.J., 1989, Edge following as graph searching and Houglr tlansfolm algorithrn for lineament cletectiol, Proc. IGARS,I'Bg, Vancouver, v.I, pp.93-96. [106] Wegleiu, 4.8., i985, The inverse scatter.ing concept and its seisrnic applicatiorr: Deaelopments in Geo1thysical Erploratiort (Metttods-6), Fitc\t T.J. (ed.), Elsevier Publishing Ltcl., pp.111-138. [107] Wenzel, F., 1988, The relation between Boln invelsiol ancl standar.d rnigration schemes, J. Geopltgs., v.62, pp.148-157. [108] Won, J.S. and Mool, W.M., 1992, Inver.sion of synthetic aperture ladar clata for surface scatteling: Geophgs. J. htt., v.708, pp.423-432. [109] Wu, C., 1976, A ctigital systern to procluce iraagely from <strong>SAR</strong> clata, Proc. AIAA Syst. Design Driaer by ,ïensot.s, Paper' 76-g68. [110] Wu, C., 1980, A cligital fast colr.elation approach to procluce SEASAT <strong>SAR</strong> inagery, Proc. IEEE I¡¿t. Rarlar Corz,f., pp.153-160. r89
[111] \,Vu, C., Balkan,8., I(arplus, W.J., ancl Carsrvell, D., 1982, SEASAT syntlietic apeltule laclar data reduction using palallel proglarrrrnable ar'- lay plocessols) IEEE T¡'a¡¿s. Geosci. Re¡note ,9en sán g, v.20, no.3, pp.352- [112] Wu, C., Liu, I{.Y., and Jin, M., i982, Modeling ancl a colrelation algolithnr for spacebolne <strong>SAR</strong> signals, IEEE Trat¿s. Aerosp. Electrott.. Syst.,, v.18, pp.563-574. 190
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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
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Ïon = _2 (V(ro) .V(¿o)+ R(ro) .A(
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: Range Walk : Range Curvatule : Ra
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olbital SAR is given by Ion = -'#{t
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is constant cluling the receiving p
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a at f¡r
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'rvith a foulula developed il this
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Chapter 4 Theoretical Development 4
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developed and cliscussed by several
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vhere u (r,ro; u) : I U 1r,ro,t)e-i
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wheÌe k':frf a¡cl lc -_ uf us ant
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4) there is relative motion of ante
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o =løo, 0, 0) Figure 4.1: Schemati
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elorv that sulface. In genetal, sul
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4.4 The Inversion The equation Eq.(
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*'here % is a platfolrn velocity an
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The trq.(a.36) cannot be used dilec
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vhele Àl is a tvavenurnbel collesp
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2-D FFT o(,b,;ø) Intelpolation in
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¡nE 0$r-sEc, ¡3 I IrlÊ [18- 5EC
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5.2 Digital Simulation Digital sirn
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Table 5.2: Moclel palametels fol di
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signal and the leconstructe
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(3 È. e tc o) o -tl a Slant Range
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that the inversiol method can accor
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(n t0 Ê) 0c (lr) Figure 5.6: Seasa
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5.3 Processing of Real SAR Data A s
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squâre pixel rvith clir¡ension of
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Aziurutì (n Þ !d !D gc Figule 5.1
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(n 5 F Þ tq Figu.e 5.11: Reconst.u
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over tlìe 2.4 inches as shol¡l i'
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Ø Þ :J m (a) (b) ^a ctl _= a"r ro
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Chapter 6 SAR fmage Enhancement for
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1) hoiv can the tlends of lineament
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6.2 Determination of Geological Str
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Coolclinates for the image space an
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Figure 6.2: Point, lines, and hyper
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scatteter (e.g. coller leflectols,
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Figure 6.5: CCRS's airboure C-band
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C-l¡ancl SAR irnagery ovel this al
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Figure 6.8: Radon transform of ailb
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in the irnage space ancl the Iine i
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ERS- 1 N U 0 rl 0o |lO + ,¡l r.l p
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6.2,3 Correlation Using The Radon T
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- Page 174 and 175: Figure 6.20: Additive irnages rvith
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- Page 180 and 181: Figure 6.24: Lnage obtained through
- Page 182: 6.3.4 Principal Components Analysis
- Page 185 and 186: Table 6.2: Con'elation coeffrcielt
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- Page 189 and 190: the geological surface lilearrent f
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- Page 193 and 194: Appendices A. Derivation of Forward
- Page 195 and 196: B. Derivation of Inversion Formula
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- Page 199 and 200: F[eferences [1] Ahmed, S., \Vallen,
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- Page 203 and 204: [43] Holn, R., 1988, E-SAR - The ex
- Page 205 and 206: [65] Lotrelrl, O., 1990, Dopplel ce
- Page 207: [87] Pye, 8.G., Nalch'ett,4.J., anc