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Appendix C Catalogue of the NRSL Radial Surface Current Data Date (1992) Zl/iO 22/10 23/10 24/10 25/10 26/10 27/10 28/10 29/10 30/10 Time (Lod) 1153 10:lO 14:17 la16 1308 1534 20:47 1031 11:12 15:18 la24 1300 17:44 09:31 10:47 10:40 13:31 0900 1309 09:30 12:W 16:06 Filename CURRAD. 29492.001 29592.001 29592 002 29692.001 29692.002 29692.W3 29692.004 29792.001 29892.001 29892.002 29992.001 29992.002 29992.003 30092.W1 30092.002 30192.001 30192.002 30292.001 30292 002 30392.001 30392.002 30392.003 Starting range (Lrm) 10.4 50.4 50.4 76.0 76.0 44.4 12.0 52.0 40.0 44.0 40.0 40.0 40.0 40.0 40.0 40.0 40.0 40.0 80.0 400 80.0 40.0 Ending range (h) 300.4 200.4 200.4 170.4 170.4 170.4 152.4 173.2 241.2 170.4 161.2 161.2 161.2 161.2 199.6 161.2 199.6 161.2 220.4 151.6 151.6 279.6 Initial Bearing '('Rue) 60 96 84 104 104 104 104 104 95 104 104 104 104 104 94 95 95 95 95 77 104 56 Final Bearing O(nue) 155 165 165 176 176 I76 176 176 180 180 180 180 180 180 165 176 176 176 176 118 176 176 FFT size 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512 512
Date Time Filename Starting Ending Initial Final FFT 1 (Igg2) 1 1 1 cmD- 1 ;= 1 ;= 1 ?&?, 1 1 size
Page 1:
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
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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 112 and 113: Where DATLOG - Array of 32x3 bytes
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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