Applications of Two-Dimensional Vidicon Photometry: Venus by Philip Henry Schaller, Jr. Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science at the Massachusetts Institute of Technology June, 1973 Department of_ Certified ht nd Planetary Sciences, May 11, 1973 by:_ Accepted by: Chairman, Departmental Committee on Graduate Students TABLE OF CONTENTS Acknowledgements ....... ........................ 2 g..................... 3 A. INTRODUCTION B. GRAY SCALE EXPANSION ............................ 6 C. IMAGE REFLECTION AND 8 D. LAPLACIAN IMAGE . 10 E. INTENSITY TRAVERSES 12 F. CONCLUSIONS References ............. Figure Captions Figures Appendix ... .............. ROTATION ................. .. .14 .... ....................... g.... o........ e .. ... ..... .. .. .... ..... ..... .. ... .... .... ....... .... .... 15 e* .... .. 16 ... 19 54 ACKNOWLEDGEMENTS I would like to thank my advisor, Thomas B. McCord, and all my friends at MITPAL for their help. Also, thanks go to R. Beebe and others at the New Mexico University for supplying their photographic plates for comparison. 3 A. INTRODUCTION The vidicon tube and the theory of its operation, and an operating camera and data system have been described by McCord and Westphal (1972). The hardware and software sys- tems have been described in detail by Kunin (1972). This thesis describes one application of the vidicon system to as astronomical problem. It has been known for some time that the planet Venus exhibits a featureless shroud of clouds in the visible portion of the spectrum. In the ultraviolet portion, however, features are visible (Boyer and Guerin 1969) Reese 1972). (Scott and These features, and in particular the curious "Y"-shaped cloud which rotates around the planet in approximately four days, are of extremely low contrast. Conventional photographic pictures are printed on high contrast paper to bring out the low contrast clouds. is The vidicon system ideally suited for this problem for three reasons. 1) The system has a wide dynamic range, incorporating many 5ray levels. 2) The system is 3) linear over this wide dynamic ranSe. The data are already in digital form. Analyses of the vlidican imaeas are simple using a computer. The yidicon images presented in this thesis were taken usinS the Kitt Peak National Observatory 84" telescope on April 23, 24, 25, and 26, 1972. The first night the instru- ment was mounted at the Coude focus. The other nights it was mounted at the Cassegrain focus. Film photographs were taken the same nights at the New Mexico State University. Thirteen vidicon images were selected for study in this thesis. These represent the best pictures at each of the several wavelengths taken during each night of the run. On the first night (the only Coude pictures) the Y-shaped cloud had apparently rotated out of view. The second night many quality pictures were obtained at .358, .383, and .402 microns. The cloud is clearly visible on this night although only one of the branches of the Y is seen. The third night only three pictures were obtained and were of less quality than the night before. The final night all pictures were taken through infared filters (see figures 1-13). Figures 14 through 17 are the best pictures taken with conventional photographic plates during each night of the run. They are all at .37 microns. vidicon pictures should be noted. Correspondence with the They also show only one branch of the Y cloud and confirm the phase of the cloud during this time. The approximately four-day rotation can be observed, noting that the cloud was rotated out of view on the night of the 23rd. These pictures, however, are not suitable for entering into the rotation rate controversy of 4 or 4.5 days (Boyer and Guerin 1969) (Scott and Reese 1972). Various image processing techniques were developed in the course of this thesis research which were used to enhance the cloud features above the background planet. The remainder 5 of this thesis is devoted to a description of these techniques and their application to the Venus cloud problem. While the data were not taken for the purpose of this thesis, a good deal of it war, usable. Although no great scientific prob- lems were solved, it is hoped that this work will be the guide for future Venus research. I B. GRAY SCALE EXPANSION To make such low contrast features such as the Y cloud on Venus more visible, various image enhancements can be performed on the computer. The first of these attempts at The vidicon contrast enhancement is gray scale expansion. system has 256 gray levels. The actual feature may extend over only tens of gray levels. These gray levels are line- arly expanded over the full 0 to 255 range. Points else- where in the picture falling below 0 are set to 0 and those rising above 255 are set to 255. As the contrast is enhanced (see figures 18-22), two effects are noticeable. 1) The size of the image decreases until under almost total contrast enhancement the image almost disappears. This is due to less and less of the image falling into the selected range of gray levels for total expansion. 2) Artificial contours are introduced by the quantization noise. When only a few gray levels are used to cover the entire range of light levels, noticeable (to the eye) distinct changes in light level are visible across the image. While the original pictures had eight bits of tray resolution, every contrast enhancement of a factor of two reduces the number of significant bits by one. Thus these contours are not inherent to the actual image (which is continuous), but are introduced by the necessity of making arbitrary decision levels in digitizing the data. Since our object data is at one end of the gray scale, a logarithmic enhancement built into the film converter was 7 also tried. (see figures 23-27) not show much improvement. The resulting images do The vidicon system also contains a routine to contrast enhance an overexposed image without loss of precision, as well as the normal overexposed image reducing routines. C. IMAGE REFLECTION AND ROTATION The usual method of mapping a feature which appears only at selected wavelengths is to divide the picture at one of the selected wavelengths by the same scene at another, but featureless, wavelength. cannot be done, In this case, however, this The scattering function of the CO2 atmos- phere, which is superimposed on the feature, is a strong function of wavelength and hence cannot be divided out. As noted before, only one branch of the Y seems to be visible on this occasion, The southern hemisphere can be divided by the northern hemisphere at the same wavelength (using the same picture, obviously), and thus eliminate the CO2 scattering function. (This assumes a certain symmetry about the function, of course.) The vidicon system now contains a routine to reflect a picture about an arbitrary axis in the plane of the picture. The problems of such a reflection on a discrete grid of points are obvious, but the results are remarkably good. Note that the proper com- bination of two reflections can produce an arbitrary rotation about an axis perpendicular to the plane of the picture. The reflected image of Venus is divided by the original and then contrast enhanced. are now immediately obvious. the reflection axis. (see figures 28-42) Two things 1) There is a symmetry about Where the image is dark on one side, it is light on the other side and vice versa. So in the same picture we have the southern hemisphere divided by the northern hemisphere juxtaposed with the northern hemisphere divided by the southern hemisphere. effect to this process. 2) There is an edge The reflection, while good, is not perfect and the limbs of the planet in the two images.(orginal and reflected) do not match up exactly. Since the light level changes rapidly across the limb, the division process greatly enhances the edge. makes it worse. Contrast enhancement The problems of contrast enhancement men- tioned in the previous section also apply here. 10 D. LAPLACIAN IMAGE Another method of enhancing low contrast features is that of the Laplacian. Being a second derivative operator, the Laplacian is not sensitive to overall reflectivity levels or their uniform variations. flectivity variations. It yields only changes in re- These are most often due to fine detail in the image. The discrete Laplacian is performed on the image by subtracting the average level of the right nearest neighbors of a point from the level of the point. (Rosenfeld 1969) The resultant values are then contrast enhanced. (see figures 43-55) The absolute values of the Laplacian may also be used for display. (see figures 56-68) Two items are noticeable in these pictures. 1) The ones taken at the Cassegrain focus show a considerable edge effect whereas the Coude pictures do not. This is due to our now enlarged raster (nine points instead of one) when taking the Laplacian. In the Cassegrain images the entire disk of the planet is approximately 32 points wide, while the Coude images show a disk 128 points wide. Since the Coude image is of smaller scale and the limb varies more slowly, the effect of the larger raster is not noticeable. One might try to circumvent this purely mechanical problem by enlarging the smaller picture in the computer before taking the Laplacian. common and both have problems, Two methods of enlarging are a) Each point is mapped into, say, four points at the same gray level. Its problem is graininess. The Laplacian pictures appear grainy enough without making them worse by this method. b) Each of the four points in the enlarged picture can be interpolated in gray level between the positions of the original gray levels. This is an expensive process and does not yield enough quality to make it worthwhile. Fre- quently, artificial contours are introduced and are enhanced by the Laplacian process. Both these methods suffer from the problems associated with displaying a supposedly continuous function on a discrete grid, (see previous section) 2) The second branch of the Y cloud is now discernable. This has been unnoticed by any of the previously mentioned methods, which shows the power of this technique. ow E. INTENSITY TRAVERSES While the CO2 scattering function is a complication for the purpose of observing the Y cloud, it is interesting in its own right. (see Appendix) This data is presented in the format of intensity traverses. The intensity of the image is scanned along a line perpendicular to the planet's terminator. All plots begin with the limb on the left and end with the terminator on the right. The organization of these 117 intensity traverses is first by image and then by latitude, In order there are nine plots for each of the thirteen previously mentioned selected images corresponding to figures one through thirteen, respectively. In each set of nine, the plots start at the northern end of the planet and end at the southern end. Note that in some cases, the first or last plot misses the planet altogether. The fifth plot in the sequence is reliably along the equator. The lines of traverse are as close to being at equivalent latitudes as is possible on a discrete grid, and very close in equivalent distance. A normalized distance scale, as well as the start and end points for each traverse, is given. Note that the traverses were taken before correction due to the mirror image reflection by the Cassegrain focus. is apparent in the absolute coordinates only. This Also note that the plots of the Coude images span about 128 points, making the Coude traverses appear smoother. For interpretation, the plots at similiar latitudes, but through different filters, may be overlayed to show the 13 wavelength dependence of the CO2 scattering function. features, such as the Y cloud, seem to be masked by the small samplinp rate when the cloud was visible. Small 14 F. CONCLUSIONS The first data from the two-dimensional vidicon photometer are at least as good as that obtainable from conventional photographic film techniques. cessin Further pro- to bring out desired features is readily and easily done through computer techniques. These techniques produce better and cleaner results With more and more sophisticated methods. The next method to be tried should be some form of high pass filtering in the spatial frequency domain. Noise filtering can easily be done along with this. Further observations of Venus with the vidicon system should span at least five nights in order to see one complete cloud c.ycle. The image should be as large as possible without reaching the edge of the target. Since the cloud feature spans just 10 or 20 gray levels out of 200, the exposure should be such that the brightest part of the image is near the top of the gray scale range. Overexposed images should be retaken, as it is at best difficult to retrieve the information. Images should be taken at several wavelengths during each night and repeated on the other nights. Adequate loggin5 of the setup of the observations and the data taken will ease the burden of the data reduction. REFERENCES Boyer, C. and P. Guerin (1969). Etude de la rotation retrograde, en 4 jours, de la couche exterieur nuageuse de Venus. Kunin, J. S. (1972). Icarus 11, 338-355. A Technique for Two-Dimensional Photoelectronic Astronomical Imaging, with Application to Lunar Spectral Reflectivity Studies. Thesis. Master's Massachusetts Institute of Technology. McCord, T. B. and J. A. Westphal (1972). Two-dimensional Silicon Vidicon Astronomical Photometer. Opt. 11, 522-526. Rosenfeld, A. (1969). Picture Processing b Computer. Academic Press, 94-102. Scott, A. H. and E. J. Reese (1972). Rotation. Icarus 17, 589-601. Venus: Atmospheric 16 FIGURE CAPTIONS North is to the top and east is to the right, unless otherwise rioted. (Planetocerntric coordinates) 1 4/24/72 Fi lter: .358 microns 2 4/23/72 .383 3 4/24/72 .383 4 4/25/72 383 5 4/23/72 .402 6 4/24/72 .402 7 4/23/72 .564 8 4/26/72 .906 9 4/26/72 10 4/26/72 1.00 11 4/26/72 1.05 12 4/26/72 13 4/26/72 14 4/22/72 "' .37 " 15 4/23/72 "9 .37 9 16 4/24/72 "9 .37 " 17 4/25/72 "9 .37 " 18 gray levels 10 to 200 of figu re 3 Notes double exposure .948 "9 "HB 1.10 microns 19 -9 60 to 200 20 "n 100 to 200 New Mexico State University "9 " 160 to 200 21 22 "f 23 figure 18 130 to 200 with logarithmic e nhancement 24 figure 19 25 figure 20 26 figure 21 27 figure 22 28 same as figure 3 29 reflection of figure 28 30 figure 28 divided by figure 29 31 gray levels with logarithmic enhancement " 10 to 245 of figure 30 32 "1 20 to 235 " 33 "o 30 to 225 " 34 "1 40 to 215 " 35 "f 50 to 205 " 36 "f 60 to 195 " 37 "f 70 to 185 38 "f 80 to 175 39 " 40 "t 100 to 155 41 "f 110 to 145 " 42 "o 120 to 135 " 43 44 45 46 47 48 49 50 o90 to 165 Laplacian of figure 1 "t Note: second branch of Y cloud Notes second branch of Y cloud 2 Laplacian of figure 9 10 53 11 54 12 55 13 56 Absolute value of Laplacian of figure 1 57 2 58 3 59 60 62 8 64 9 65 10 66 11 67 12 68 13 FIGURES 20 Figure 1 Pigure 2. Figure 3 Figure 4 2Z Figure 5 Figure 6 Figure 7 Figure 8 Figure 9 Figure 10 Figure 11 Figure 12 26 Figure 13 Figure 14 Figure 15 Figure 16 26 Figure 17 Figure 18 29 Figure 19 Figure 20 30 Figure 21 Figure 22 Figure 23 Figure 24 3z Figure 25 Figure 26 33 Figure 27 Figure 28 3Sf Figure 29 Figure 30 35 Figure 31 Figure 32 36 Figure 33 Figure 34 3? Figure 35 Figure 36 38 Figure 37 Figure 38 39 Figure 39 Figure 40 40 Figure 41 Figure 42 4' Figure 43 Figure 44 42. Figure 45 Figure 46 Figure 47 Figure 48 44 Figure 49 Figure 50 45 Figure 51 Figure 52 %I' Figure 53 Figure 54 Figure 55 Figure 56 SjB Figure 57 Figure 58 i9 Figure 59 Figure 60 Figure 61 Figure 62 Figure 63 Figure 64 51- Figure 6.5 Figure 66 53 Figure 67 Figure 68 APPENDIX z,-. I- z ~48 8 8M.00 0. 0.10 PC o.30 a'1o 329.0 .50 PGSIT ION 0. w 0.70 0.80 0'.90 121.0 1'.00 153.0 VENUS FILT=.356 EXP-.42 4/24/72 926 PRL217 009 >- p zi 8. .0 .0 O.0 0.30 O.50 C.40 rS 133.0 0.60 0. 70) 0.30 I TIN FILT=.35 EXPw.42., 4/24/72 t0 165. D IWO0 117.0 VEtIUS 0.30 928 PRL217 009 VD43S0 )J 28. 8" I C LI I 7 u.a0 137.0 113.0 .o10 U 0.20 .. 6.0 1 .4o0 * 0.so PSIT ICN o-.o -I 0.y 7 o'. 0 0.o 16.0 15.0 VENUS FILT=.3G& EXP-.42 4/24/72 928 PRL217 009 Veases b" I- c.oo .o.i 0.10 0.,0 0... 0si 0.60 U.,0 -- O POSITION VENUS FILT.36 EXP~-.q2 4/2q/72 0.90 1.0 373.0 141.0 141.0 928 PRL217 009 veoses cr 84 *z 8.D 0.g i'.o 1m7.0 137.0 VENUS FIL7=.3S EXP-.42 4/24/72 928 PRL217 009 .. 8 1 Vees 0 8 4~4 U, z lii I-- F. z 0.730 2419.0a 101.0 VENUS 0'.50 POS1I71GN FILT=.356 EXP-.12 4/24/72 1is.0 928 PRL217 009 58 B. 2:'lii I2: b.42 S -D.00 0.20 0.10 o.so n.so POSITION o.Wo 0.70 o.so o.s 1~.o 12a.o 07.0 VENUS FILT=.3S8 EXP-.42 4/24/72 928 PRL217 009 vueses 'IJ I-- 8 0.10 0.go 0.3 0.40 167.0 0. POS1TIGN 0.60 0.70 Owo 1.00 109.0 83.0 VENUS O.no FILT'.356 EXP-.42 4/24/72 928 PRL217 009 Von SIM 59 B :i. 4 1AJ I-. zb.48 S B ,-. ---.-.------- ____ l' 20 0'.s0 0'l .w 261.0 09.0 -. O'.so POSIT ION d. w 0.70 .so .go 19'.0 121.D3 VENUS FILT=.356 EXP-.42 4/24/72 928 PRL217 009 B. VEeWSa tz -d.jo - 020 0.30 0.11 J37.0 0.60 0.70 0.90 090 1.00 1,.0 J37.0 I69. YaH06 O.50 POSITI0Mt FI LT=.383 EXPA4,0 4/23/7Z 1000 PAL216 018 - 60 8. %.n ot a o 0.10 o'.so wn .70 o.so w~ I'. POSI TION 147.0 153.0 VENUS FILT=.383 EXP-6.0 4/23/72 1000 PRL216 018 . -D ..... l 8~ 8 0 n o.00.co t3.sJ 157.0 sv~oPGSi 0.10 O.so 0.5 0.70 T7 1ON FILT:.3U3 EXP-65.0 4/23//2 1086 0.9. 6I1.1 137.1 V1N11S1 0.80 PRIL216 a018 VtM651.4 61 8 u6i 8 8S. '~8 Wbao o.lo . o'.o o' 0.20 o'.50 1st~o POSIT ION .o .1G 1'.' .ow .su iei~o VENUS .a 71.0 - o.0 FILT=.363 EXP-6.0 4/23/72 1000 FRL216 018 -0 S zn ~8. i.oa 0.10 0A~g 0.so 0.4L0 O.!o 0.60 0..0 0.80 0.9 rr,.o VDIJUS 7 1.0 73.0(I It 15Ir .33- fXP-6.0 4/23/72 1000 PAL216 010 -D 62. 2 0"I uJ 5z 88 0. .0.0 POSITION01.0 187.0 89.0 s?.0 VENUS 4/23/72 1000 FILT=.383 EXP-6.O PL216 018 "I * -'F) (;)Iu, lq I I.- 8. 1', * *1 Ii. i~*' hi. ~ INIC I 1~ ,.t~ vLT~1.) I J J 0.~n f.il. i ~; 1.~r3 1~'7.it I 111' 1 :' j, " -l tI 13 .-n- 63 z-en- S- 93.00 0.10 0.20 0.s0 0.10 0.30 FILT=.383 EXP-6.0 VENUS . .0c.80 4/23/72 1000 0.70 0.80 PRL216 018 0.90 1.00 -D3 to 8 F8. en- z- '.if o. o f.e U.Nal u.fu U.60 0.71 0.80 0.9. P03'rifeS.,. 'ii .u %fViNiIt-, 'I-30'PXP-.31/53/72 1 PRL-216 018 --) 64 V"0o3C 8 8 POO.,I7 1ON 121.0 '113.0.15. FILT=.383 EXP-.1 S VENUS 4/24/72 923 PRL217 O0 8- X.- U.I() )~'!~. fl )(f~i. Li V It Kil; OA~fl (I. 3n 0. 410 0.Gil P '0,31 UIjN CD 0.*70 0.0)0 ,. Ltyj y 1 '*. VoEsse 65 8 I 13 8 <.4-- -- -_________ I"b.a 0.2 0 o.wo .o w o.sa POSITION 129.0 105.0 . . w .70 0.ea 0.s 1.00 157.0 VENUS 4/24/72 923 PRL217 00S FILT=.383 EXP-.15 z-. 1II3. ; in. l 1'i ~ e I '1i . E.XPs'i - . I 4 /-1/i nn -w 1.6:-m n'.:nI' u.n Ii, u.so .0 tr:,. r :. PH 1'/ 005 66 157.0 " "'' VENUS ul z-- FILT=.303 EXF-.1S ''% '. 4/24/72 . 923 em.o - FRL217 005 -0 .- ] .L0 0.10 0.20 0.30 0.40 0.50 POSITION17. 0.60 0.*0 -- 141.017- VB.I Ili F L .:.33 X-.15 4l/2.:i/72 92c'3 PF1L217 005 O.0 O.E 1.L 177.0 121.0 ga.0 59.0 VENUS FILT=.383 EXF-.IS- 4/24/72 923 PRL217 005 8 vDesse S B 8 POSIT I CN 19. 0 VENU'ji -fl 117.0 FILr=.365 EXP-.1! 4/24/72 b23 FAL217 L005 vecese Uzj 8L 8z '10 0.0 o.e . 53.0SIION 51.0 .70 0.80 0.90 1.0 . 113.0 FILT=.383 EXP-.1S VENUS 4/24/72 923 PRL217 005 8. 8J 8 .- 9sc. o 0 .10~~ao f.0 0n ~ir] PG(1'110N 0.e 0.' . 21?.n VDIUS I 80Te 0.0 I.00 ei.n FILT=..3= -3 XP--.14 4/i5/72 9o FRL218 071 . 69 &-4 D.co 12.0 oao 0.!0 0.9 f'(S1TI ON VENUS FILT=.383 EXF-.L t 4&/2S/72 2.0 110.0 902 FARL21EI 071 - cSf .8 0. Mo cbo Gf D 01 P031 T 1 i . VFl.4LJfll VEUU5P--Il FqlT.~sl 1L i 2 90? rAL210 071 veessa 0.20 .so 0.. 0 0.6. POSI TION sea.0 129.0 VENUS 0.0 0.so .1a FILT=.363 EXP-.l t 4 1ie.0 03. 4/2S/72 902 PRL218 071 yeeam 'Vil VENI Is o.so o.'a o.'rs o.co 0.70 o.60 0.90 PO(317 1 ON FILT=.3P3 EXP'-.14& 41/2'L/72 902 FRL210 071 -- -.c0 - ees. 71 21 .0 ' "'' 1111.0 141.0 ' ' ' 137.0 FILT=.363 EXP-.4t t VENUS 4/25/72 902 -0 FAL218 071 8 8 . a,.iu 0. M .w P..sa FA L'D'83 E0.l' 0.70 PQSJ3"'-~ 147.0 )u).13 4 /25/72 902 PRL-216 071 .81 0.9 1.no ^ 72 8 8I'13 8B 8 ' | c.no u.lo ' ' . w .o w .w 10&.0 14o.0 VENUS d.co .m POSIION a.so d'. w t'.00 11r.0 14s.0 FILT=.363 EXP-. 902 I& 4/2S/72 FAL210 071 -D I-. zw-. uJ F- ufl1.0 0- 1 [. 117.0 vin.n VER BS 191-0 FI ='MEXP--14l 14/1-:1/72 9,1.2 PTIL2163 071 vecD2C >-B z-. 8 8 8 .to . 20 .o30 153.o FILT=.402 EXP-1.0 VENUS Pd S ITIN o.so 4/23/72 1002 --- I- 0' m 0.a w 0.s 67.0 137.0 PRL216 020 veaO#c tu I-- 28 8 0.7U 153.0i VDBJUS 1 0.0 0..L I I(1. V1Th43'i FILi:~.Lifl~ LXS'-~1 .0 tj/~.)~j'7,3 ~flji I'.m rnL'~I5 020 P11Lc216 --0 0 Va,4O2C ruL 1 LUN 173.0 137.0 FILT=.402 EXP-1.0 VENUS 77.0 4/23/72 1002 -0 PRL216 020 g.venoac . 8 ha z- 8 . 0..0.70 ..... 0.0 0.no POSH7 1 VENUC~ rILTh.4C2 EXP-1.0 4/i3/72 1. a7.0 1002 P14L216 020 -0 VenOPC 75 >.co VE6.0 97.0 73.0 VENUS FILT=.402 EXP-1.0 4/23/72 1002 PRL216 020 8~ 8 (- z .M tIj 8 8 a~m 7u nas otwo 7 P7.0 00.0 Fil T=.4ti2 EXP-1.0 4/23/72 1.012 PHL216 020 - IM.- VENUSJ FILT=.'I02 EXP-1.0 0.2uP oIee12 '/23/72 1002 IrFL216i 020 O . 67. FilT.m.(Th,2 EXP--1 .0 4/~23/'12? 10J2 020 FAL.216 rL 600- -0 77 Bn9 z 9 .a o. io Go ol w o~o 0.110 d. -M DOS5IT ION d.so 137.0 9.0 I1.0 IILT=. 1102 EXF-1.0 VENUS '&/23/72 1.002 12AL216 020 vemaoam 8vBu f-7.1--.----------- 9J~o0.10 0.~1 fly) fl.1~POS 17 1 ONt~1 7~0.J vIt Y.'; 09 AM;3. L' i r..n )fl?.rs IM.0 FIL'I'--. 110? ['Xl'-. (13 FAI PRI.P.17 023 v~emOA 78 8.Lu 81 :81 '.oo 0.10 .o a o. W M~.0 7.0 VENUS POSITION . .5 .io.70 o.o 'w- -. 0 lES.o FILT=.402 EXP-.03 4/24/72 947 PRL217 023 z 8- In P~.0 V'(45 ~. ELM U.1'1) T 1N 4/24/7P 157. ,3 £47 PRL2J17 023 79 8* lLi 8. I' 8 CV. w 0.o 0 . 20 d.0 0. a. w so Pc(SI TION 1.0 0. w 1-70 0.30 0-so0 I.c0 161.0 121.0 VENUS 4/24/72 FILT=.402 EXP-.03 947 PRL217 023 VEME0A in- z zj 8 8 S2r1 DADO PS I o 0.76 .0 20 117.0 -I". VE NUS5 .3 1.0 N FIVfIi.LT-r.2 LCXP-..03 4/241/72 947 PFIL217 023 - vool" 80 137.0 51.0 VENUS Ues.0 211.0 FILT=.402 EXF-.03 4/2'i/72 9L&7 PFL217 023 veft"O /u(t P)11.0 77.0 v['01-11i Viii*~f'~ IiU; . 1,1- Yt.O~ iWj1/4 ijtf7 I'lull' ( 123 81 8 z - coO 0.20 o.go 0.so 0.no 0.so 1.60 0.70 . w .o 2'.00 P1SIT1ON )tus.0 Uas. 0 75.0 FILT=.402 EXP-.03 VENUS 4/24/72 947 PRL21 7 023 VD4Mo 8 8- 9.| Ch.un 0.lo a.e -nau 1,10" V.5 NOc U7.;- 000 S1.n tLco 181.3 2tUl.L FaLO VLtNUS 1 0.so iil.: .4 D:P-- [x .039 /4/~/ f17 rL.217 23 82 8 %I- 2nR 81 930cc ~----I 0.20 I 0.~0 '.o '.50 29.0 27.0 VENUS FILT=.56I EXP-.20 d.so POSITION D.)o .?o .w .so W5.0 MID. 4/23/72 1011 FRL216 027 ~8. . 8- 98.m 23.0 23;.'J' T~ O.r'LI -~~~1--~ .LO u.roi Co.( P(Y31 1.o 0.70 1oo O.N T PRL216 027 (sNs59 -O 83 141.0 115.0 77.0 FIL7=.564I EXP-.20 VENUS 4/23172 toll PRL216 027 -0 ve6Sa i'.inl 141-0 V1-OS~1 . -- - ~.- T-- G-I-'.O'm g tj~g// 11 r1L216 027 84 POSITION IS&o 57.0 65.0 ee.o VENUS FILWT.564 EXP-.20 .UU~~~ ~ I M),0 4/23/72 1011 FRL216 027 71 W 5.01.3 1.00 Uii.Ll I. 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VENUS5 FILT=.906 EXt~-.03 '1/25/72 0000 FARL219 110 MEel5A w F- 117.0 vPjlj(5 .IZ Ga0D nAu05 V Ft'J~3 l'LT=. 5,5 I'Xr'-. 03 //? 000~f) , P14.21 9 Ito Vr.mSDmA 8/ 8-. 8J, 8- 8 .ow 0'.10 o.o o.so o.3o o.ao .70 POSIT ION 119.0 0.S t'. o -1.00 87.0 139.0 FIL7=.906 EXPA-.03 VENUS 4/26/72 0000 PRL219 110 VM,5a I-z . 0.10 9.00 Vwit VDUS 0. o.3 FILT:-.06 0.110 0.!71 0..0 PTSw FITZ 11- ^Xi'--.03 o.sgr 0.70 0.50 1 iOO~L1 /237 4/Lr5/712 C00 PRL21 9 110 0.Do0 001 -D 1.00 ,, nU VDoMW 89 0.0 o.a i0'.30 - .- ir-- 0.1o 0.50 . O.60 0.90 PMSIT ION FILT=.906 EXP-.03 VENUS 0.90 1.00 ,1.0 4/26/72 0000 FRL219 110 8. . 8 cb.c ~ 0.10 0.20 0.3 0. 0- 0.6b .70 0.80 Ctr05- I w 3.0 14);.t] VLl 11S 157.0 4/? 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