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Where DATLOG - Array of 32x3 bytes representing i"p logistic informstion such as site loeation and time of data collection BORSIT - Receiw antenna boresiteis 'BORSIT degrees elockarise from Th~e Nonh.(REAL*4) RANGE - Array of 3 (4-byte) red value where RANGE(1) - Distance to middle of k t range annulus (km) RANGE(2) - Distance to middle of Lsst range mulul (h) RANGE(3) - Rage annulus width (km) NFET - FFT size used to generate file (INTEGERe4) NFIELD - Number of fields in data file format. Far thi. data set NFIELD=2 (one for the radial velocities estimate md one for the SNR values). (INTEGER-4) LEEAR - The last bearing processed. This bearmg indicates where the processed data begins . i.e. RAD(i) is from bearing LBEAR, RAD(2) is tom bearing LEEAR+l. RAD(3) is tom bearing LEEAR+P, ete. Each remaining reeord can be accessed as shoaa in the following example Let NRANG - Number of range snnulli p r o d NANG - Number of angular bins (max. of 360)
RAD(360,NRANG) - (Real-4) array of radial velocity valuer SNR(360,NRANG) - ... and their SNR valuer. The Wrtran code is a~ follows: STANG=-LEEAR+IIO STlNDEx=MAX(l,~(STANG,360)) DO IRANG=l,NRANG LREC=IRANG+l READ(LUN 'IREC)(RAD(I,IRANG),I=ST~EX,ST~Ex+NANG) IREC=TT(ANG+NRANC+I READ(LUN 'IREC)(SNR(I,IRANG),IsST~DEX,STmEX+NANG) END DO Notes: By the way. NRANG = (RANGE(2)-RANGE(l))/RANCE(3). The variable BORSIT m y not be correct in the data 6le header. It should be the value 121. In any ease, it doesn't matter what value is there. The proper borerite value is incorporated in the data reeord structure.
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CENTRE FOR NEWFOUNDLAND STUDIES TOT
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Abstract Esrlm=r#oo of ocean surf-
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Acknowledgements Quite a number of
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Contents Abstract List of Figures L
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5.2 Direct Radial Surface Current C
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3.4 System architecture of Cape Rae
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List of Tables 5.1 Summary of stati
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List of Symbols d : Distance irom r
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Chapter 1 Introduction The monitori
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southward. In t k example the same
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1.2 Conventional Methods for Measur
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iceberg motion, a better relationsh
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magnitude of the radid component is
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Rice 1241, Barrick [I] developed an
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ange broad and narrow-ham systems (
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the shon-r- radar is quite diEerent
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of a chapter. Thig dso provides an
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2.2 Radial Surface Currents 2.2.1 T
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Figure 2.1: Radw Spectrum (solid li
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intervals of Ar and A.9, where thee
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Figure 2.3: Wan Q is mbdivided into
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The abwe system of equations is swe
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Chapter 3 Experimental Data 3.1 Int
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e built at other eoastd sites such
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Since the mean currents within mast
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Figure 3.4: System architecture of
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spatid variability and to check sys
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oth of these techniques ean then be
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the dominant, or 9-, peaks of the s
Page 62 and 63: modelled, since they are known quan
Page 64 and 65: Sine the drifter estimates m e mnst
Page 66 and 67: 4.6.2 Selection of Algorithmn Param
Page 68 and 69: subtended by the b- increases in sb
Page 70 and 71: simplib the analysis by converting
Page 72 and 73: for then beams is therefore 3, 5 an
Page 74 and 75: with the graphs are from a linear r
Page 76 and 77: Fiere 5.2: Scattergrams of radid su
Page 78 and 79: Table 5.2 that the SNR eases of 10
Page 80 and 81: m-ments deliwred by radar and buoys
Page 82 and 83: Figure 5.6: Scattergrams of simulat
Page 84 and 85: Figure 5.7: Scattergrams of -tor me
Page 86 and 87: size. In other words, the algorithm
Page 88 and 89: tem, which is a programmable fsture
Page 90 and 91: Radii vetocify [cws) - Radar Figure
Page 92 and 93: ocean surface m nts where the curre
Page 94 and 95: Chapter 6 Conclusions 6.1 Direct Ra
Page 96 and 97: gential component estimate, wen wit
Page 98 and 99: One of the goals of this thesis has
Page 100 and 101: Future work dl also deal with the f
Page 102 and 103: [I4 D. Diemand, E. Faemer, and J. B
Page 104 and 105: (461 D. Barriek, M. Evans, and B. W
Page 106 and 107: DATE (LOCAL) EVENT Comments shorn 6
Page 108 and 109: TIME - DATE (LOCAL) EVENT Comments
Page 110 and 111: The tape was mated by using the DEC
Page 114 and 115: Appendix C Catalogue of the NRSL Ra
Page 116 and 117: Date (1992) 11/11 12/11 13/11 14/11
Page 118 and 119: Time I FFT 1 - Date 01/11/92 02/11/
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