Pacific University CommonKnowledge · 2020. 1. 28. · Wyszecki goes into a detailed explanation of...
Transcript of Pacific University CommonKnowledge · 2020. 1. 28. · Wyszecki goes into a detailed explanation of...
Pacific University Pacific University
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College of Optometry Theses, Dissertations and Capstone Projects
8-24-1974
The affects of tinted lenses on visual dection of features in a The affects of tinted lenses on visual dection of features in a
snowy environment: A computer simulation snowy environment: A computer simulation
Lynn Burge Pacific University
Recommended Citation Recommended Citation Burge, Lynn, "The affects of tinted lenses on visual dection of features in a snowy environment: A computer simulation" (1974). College of Optometry. 372. https://commons.pacificu.edu/opt/372
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The affects of tinted lenses on visual dection of features in a snowy environment: The affects of tinted lenses on visual dection of features in a snowy environment: A computer simulation A computer simulation
Abstract Abstract The affects of tinted lenses on visual dection of features in a snowy environment: A computer simulation
Degree Type Degree Type Thesis
Degree Name Degree Name Master of Science in Vision Science
Committee Chair Committee Chair Frank Thorn
Subject Categories Subject Categories Optometry
This thesis is available at CommonKnowledge: https://commons.pacificu.edu/opt/372
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THE AFFECTS OF TINTED LENSES
ON VISUAL OECTION OF
FEATURES IN A SNOWY ENVIRONMENT:
A COMPUTER SIMULATION
THE AFFECTS OF TINTED LENSES ON VISUAL DETECTION
OF FEATURES IN A SNOWY ENVIRONMENT:
A COMPUTER SIMULATION
Lynn Burge
Submitted in partial fulfillment of the requirements for the degree
Doctorate of Optometry
August 24, 1974
Approved by Advisor
ACKNOWLEDGMENTS
I wish to thank Dr. Frank Thorn for
his help and guidance in the prepara
tion of this paper. Also, special
thanks to Dennis Olson of the Pacific
University Computer Center .
TABLE OF CONTENTS
INTRODUCTION
HYPOTHESIS AND THEORY
PROCEDURE AND PROGRAMMING
RESULTS . . .
Table I - A & B Luminous Contrast
II - Color Contrast Enhancement
III - Color Distortion in CIE Space
DISCUSSION
BIBLIOGRAPHY
APPENDICES
A - Listing of Computer Ratios Programmed
B - Luminous Contrast and Ratio # 2
C - Spectral Transmission Curves . .
1 1 3 5
6-7 8
9
10
12
14 15 17
INTRODUCTION -'
A computer was used to anaiyze various colored tints
of sunglasses to, theoretically, see if any special tint
would enhance contrast on snow .
Any appreciable increase in contrast could make sudden
changes in elevation such as crevasses, fissures or ditches
easier to detect by people driving or skiing on snow . A fast
skier needs as much advance warning as possible for changes
in snow elevation. This situation is extremely important for
the conditions of an "arctic whiteout" where all of the snow
features appear to have the same whiteness. 'Ibis condition
is represented by uniformly overcast sky .
HYPOTHESIS AND THEJORY
Several assumptions have to be made to treat this
problem by mathematical procedures. The basic assumptions
followed were those set forth by Wyszecki .1
The "arctic whiteout" is represented by a uniform
overcast sky and a completely diffuse reflecting snow sur-
face .
1G . Wyszecki, L._Opt. Soc. Am., Vol. 46 (No . 3), 1956.
1
The sudden changes in elevation considered dangerous
to a driver or skier are represented in Figure One . Type
2
(1) is a ditch with a unit width and a depth of 1 times the
width . Type (2) is a 11crevasse11 with unit width and "infinite"
depth . Type (3) is a "step" of unit height . Type (4) is a
depression represented by the angle�. The step, ditch, and
crevasse as represented have infinite lengths; in other words
their lengths are many times longer than their widths .
The observer sees the snow surface from an angle$ in Figure One. This angle q, of about 27° (Tan + = 0 . 5)
compares to a distance between the observer and snow edge
of about twice the height of the observer. This is consid
ered to be the lowest limit at which a driver or skier should
detect an elevation change.
An observer looking at angle f will only be able to
detect a change in elevation if some surface elements appear
to be perceptably different in brightness or chromaticness
from the horizontal surface of the dangerous feature . It
would be expected that the surface hollows would be darker
and appear bluer compared to the reference surface because
only parts of the overcast sky illuminate the interior sur
faces and also because of the inter-reflections between the
walls of the hollows .
Wyszecki goes into a detailed explanation of the
formulas showing the spectral reflectance of snow (p) and
luminous ratios [r(s)) as functions of wavelengths. These
formulas are listed in Figure One alongside of the respect-
ive hollows they represent. Figure Two shows the resultant
graph of the above formulas. The spectral reflectance of
the snow surface (p) immediately beneath the observer is
3
compared with the reflectance r(s) of the point in the hollow
he is observing. This forms a contrast ratio.
The graph in Figure Two leads to the hypothesis that
a shift to a higher wavelength or towards the red spectrum
will increase contrast. This is illustrated by exaggerating
the contrast ratio as in Figure Three. Contrast is defined
as p-r . It can be seen that p decreases rapidly and p-r p
decreases at a much slower rate. Thus as a point is chosen
further to the right on the graph the contrast ratio increases.
PROCEDURE
The four hollow conditions were analyzed on a computer
for nine tinted lenses. Ratios were programmed to anlyze
p (�) and r (�) functions to compare the luminance and
chromaticity of the observed colored surfaces.
4
CD ru ( s) = (A�) [A1 Co sh (ks)+Az . Siri H . (ks]
0.2
® : , __
®
FIG. 1. Cross sections of four types of sudden chan"es of elevation in a snow field. · 0
400 600
;i.· [mµ.]Frc. 2. Spectral reflectance of snow and luminance·n
functions of wavelengths. The cun:es indicated by 0, 11;.1 3, 41, 4z represent p(f.), ru(f.), etc_ ;
p
r
I ! !
a.! bl__ A
Fij . .3. Coriira.sT Ra..t1·0
rz(s) ;;:::
r3(�) =
r4 (s) =
A0 = 2 cosh (kl)+k[l+(l+p) sin h (kll} .
A1 =
Az =
p (Cl+p) cosh (kl) +_ k sin h (klj -p((l+p) sin (kl) + k cosh (klJJ
1: k = (1-p) 2
r11 O) Ditch t;..., 0.5
(1-k) exp (-ks)
1 = 1.0 1 = 2.0
0. Sp L 0. Sp (l+p) (1- Cos.) (1 +cos� �
2 . . p sin a/ (1-p cos2 a)
+
FIGURE 4 Color of Snow Surface viewed through Tinted Lenses 4b
900 900 . . .,- . . I ,...., I .
- '20 ,, 525
515 , / . 530 � . 800 800
r 5� l I I "' � OJ I ,..,, 540 " .... \i'l.. M&
I I I '' I I I 5!50
I I roo 700
'I 5
' .600
500
I ' .500
y 495
.400
� - ' w _:;oo 490-••
.200
-480
.100 �
475
-
000 I h
§
.... '! 555
I I 580 I " .... I I I 1\565 I I I I • I
I I I I j I I
I I I I
I
1 or I ,, I I
� I I I
I
I
I
I I
I I
I �10 " •
-
41& ' 460" I 45!1 � 4�40-� ...... I
420 -x
0 Poloroid Neutral A B&L Smoke # 4
I
8 Cool Ray blue/green X Doc # 2
I
I I M
I I
I
EBAO Rose Smoke, medium O Nov C 6 Poloroid Yellow CJ Wratten 23 X Wratten 16 lP (no filter)
"" I
I
.....
•ro j ��r. • ,.,.580 I I ! l I � i I H
I ·;-., SIS
� [± �-+ :f�s.c ;: .. .. I ·- I I
( I I �
I I I I I I •
I
I I _,...
I �
I
i I
-·
....
I I I I i
·-
- 605 :ib 610 1 ... �,&I 620 I ·" 630 I'\.�
� � ��� .. "'°
I I I l I 1
0 R
600
500
y
400
300
200
-- .100
.000 �
5
Using the color mixture functions of the CIE standard
observer representing the eye and the relative spectral
energy distribution S (�) of the overcast sky, and the CIE -
tristimulus values X, Y the CIE - chromaticity coordinates
x, y may be calculated for each given p (�) and r (,\) condi-
tion. When tinted lenses of spectral transmission 'YC/t) are
used for sunglasses the same procedure is performed for the
functions,...(�) p (�) and 1" (�) rs (�) .
RESULTS
The spectral transmission curves of each tinted lens
are shown in Appendix C. Table One represents the luminous
contrast ratios for nine tinted lenses for each of the snow
elevation conditions. Columns 3 through 9 show the lumin-
ance difference4 Y = Yp - Yr relative to the luminance Yp
.
Table Two represents color contrast enhancement . The
apparent color contrast enhancement between the snow surface
and hollow feature is shown by � = x p - X.:r and y = y - y . p r
Table Three shows color distortion in CIE color space.
Color distortion is how the tinted lenses change perceived
color. This calculation is shown by x shift = X (filter) -p
xp (no filter); y shift = Yp (filter) - Y (no filter); p color shift = J X�h+ Y�h The color of the surface of the
snow viewed through the various tinted lenses is shown in
Figure 4, page 4b .
TABLE IA LUMINOUS CONTRAST Illumination: Heavy Overcast
(1) (2) (3) (4) (5) Elevation Conditions Rl-Ll Rl-L2 Rl-L3
Wratten 23 .3690 .3963 . 4114
Wratten 16 .3607 .3882 .4038
Doc 2 .3598 . 3873 .4029
Polaroid Yellow .3564 .3841 .3999
AO Rose Smoke, Medium .3557 .3833 .3992
Noviol C . 3542 . 3820 .3980
B&L Smoke # 4 .3527 .3804 .3965
Cool Ray blue/green .3521 . 3798 .3959
No Glass Filter .3517 .3794 . 3955
Polaroid Neutral .3509 .. 3786 .3948
A y = y - y p r ---
y p
(6) (7) R2 R3
.4790 .0208
.4727 .0200
.4720 .0199
.4695 .0196
.4689 .0196
.4678 .0194
.4667 .0194
.4661 .0193
.4659 .0192
.4652 .0191
(8) R4
.1982
.1917
.1911
.1884
.1879
.1868
.1857
.1851
.1848
.1842
°'
TABLE IB
(1) (2) Elevation Conditions
Wratten 23 Delta Y
Wratten 16
Doc 2
Polaroid Yellow
AO Rose Smoke, Medium
Noviol C
B & L Smoke # 4
Cool Ray
No Glass
Polaroid Neutral
LUMINOUS CONTRAST Illumination: Light Overcast
(3) Rl-Ll
.3685
.3603
.3591
.3562
.3553
.3541
.3525
.3518
.3513
.3506
(4) Rl-L2
.3958
.3879
.3866
.3839
.3830
.3817
.3802
.3796
.3791
. 3 783
(5) Rl-L3
.4109
.4035
.4023
.3997
.39'89
.3977
.3963
.3957
.3953
.3945
(6) R2
.4786
.4725
.4714
.4693
.4686
.4676
.4664
.4659 .
.4653
.4949
(7) R3
.0208
.0200
.0199
.0196
.0196
.0194
.0193
.0193
.0192
.0191
(8) R4
.1978
.1914
.1905
.1882
.1876
.1866
.1854
.1849
.1845
.1339
-.....J
TAB LE II COLOR CONTRAST ENHANCEMENT Heavy Overcast
� = x - x p r y
= y - y p r
Doc No . 2 4 x �y
B&L Smoke No. 4
No Glass Filter
AO Rose Smoke, Med .
Cool Ray, blue/green
Poloroid Neutral
Nov C
Polaroid Yellow
Wratten 16
Wratten 23
Rl-L3 Rl-L2 Rl-L3 R2 R3 R4
.01002 .01029 .01000 .00946 .00059 .00613 .00667 .00692 .00677 .00642 .00039 .00404
.00760 .00781 .00757 .00717 .00045 .00466 .00604 .00629 .00618 .00586 .00035 .00364
.00741 .00761 .00739 .00700 .000445 .00455 . 00652 . 006 77 . 00664 . 00630 . 00038 . 00395
.00727 .00745 .00722 .00683 .00043 .00444 .00327 .00343 .00338 .00320 .00018 .00195
.00711 .00729 .00707 .00669 .00042 .000435 .00436 .00454 .00447 .00424 .00025 .00262
.00701 .00720 .00699 .00662 .00042 .00430 .00652 .00678 .00665 .00631 .00038 .00395
.00524 .00534 .00515 .00436 .00031 .00321 .00195 .00196 .00188 .00177 .00012 .00121
.00381 .00387 .00371 .00351 .00023 .00234 .00340 .00344 .00331 .00312 .00020 .00209
, 0023 7 • 00239 , 00229 • 00216 • 00014 • 00146 I
.00230 .00233 .00223 .00210 .00014 .08141 ':' . 00066 . 00066 . 00063 . 00059 . 00004 . 00041
.00066 .00066 .00063 .00059 .00004 .00041
1
2
3
4
5
6
7
8
9
TABLE III
Color Distortion in CIE Color Space
x shift
Polaroid Neutral -. 0082
B&L Smoke # 4 .0258
Cool Ray blue/green .0357
Doc # 2 .0823
AO Rose Smoke, Med. .0966
Nov C .1252
Polaroid Yellow . 1742
Wratten 16 .2253
Wratten 23 .3343
x shift = �p (filter) �p (no filter)
x shift = Yp (filter) - Yp (no filter)
color shift = \l(x shift�f + (y shift7 illumination = Light Overcast
y shift color shift
.0065 .0105
.0401 .0477
.0822 .0896
-. 0378 .0906
.0914 .1330
.2009 . 2367
. 2135 .2755
.-1719 .2834
.0652 .3406
'°
10
DISCUSSION
The R3 condition has very low luminous contrast; the
other conditions are above incr-emeiit thresholds . However, for
the skier or the pilot corning into this type of condition at
high speed, he must have quick reflexes and any enhancement
of contrast is useful .
This paper is looking for filters and tints which
will maximize contrast. Overall the lenses studied gave
discouraging results in contrast enhancement. Wratten 23
and 16 gave the most enhancement in luminous contrast and
this was only 4-8%. Contrast is enhanced slightly by tints.
This may be useful for someone who needs a racer's edge. For
the casual skier the contrast enhancement would probably not
provide any noticeable improvement .
It is interesting to ask if color contrast offers
assistance in seeing the difference in snow elevations. Color
enhancement is by far the best for the Doc lens . The Wratten
filters, which did good with luminous contrast, destroy color
contrast .
The Doc lenses seem to combine both color contrast
and luminous contrast so that in overall contrast enhance
ment it was the best lens .
11
We should ask about color distortion. Does the world
look natural or distorted? If it looks unnatural, will off
color tints effect the involved person's reactions .
The color shift is very great for many of the lenses
which enhance luminous contrast or color contrast . The Doc
lenses have the least amount of color distortion when
compared to the lenses which greatly enhance contrast .
12
BIBLIOGRAPHY
Eastman Kodak Company, .Kodak Wratten Filters for Scientific & Technical Use, 22nd Ed., U.S.A., 1968
Stair., Ralph "Spectral - Transmission Curves," National Bureau of Standards, Circular 471. Washington, Government Printing Office, 1g4g
Wyszecki, Gunter, "Theoretical Investigation of Colored Lenses for Snow Goggles," Journal of the Optical Society of America, Vol. 46 (12), December, 1956.
APPENDICES
A - Listing of Computer Ratios Programmed
B - Luminous Contrast and Ratio # 2
C - Spectral Transmission Curves
13
APPENDIX A
Listing of Computer Ratios Programmed
Ratio = Luminous contrast ratio = Yp Yr Yp
14
value greater than one indicates contrast enhancement
llY
x r
= y - y p r
Ax ratio = Qx(filter) Ax(no filter)
x shift = x (filter in) - x p x shift = yp (filter in) - y
(no filter) p (no filter) p
Color shift = '1{x shift)2 + (y shift)2
APPENDIX Bl LUMINOUS CONTRAST Illumination: Heavy Overcast
Elevation Conditions Rl-Ll Rl-L2 Rl-L3 R2 R3 R4
Wratten 23 fly .3690 .3963 .4114 .4790 .0208 .1982 Ratio # 2 1 .049 1 .044 1.040 1 .028 1 .082 1 .073
Wratten 16 .3607 .3882 .4038 .4727 .0200 .1917 1.026 1 . 023 1 .021 1 .014 1 .041 1 .037
Doc 2 .3598 .3873 .4029 .4720 .0199 .1911 1 .023 1 .021 1 .019 1.013 1.038 1 .034
Polaroid Yellow .3564 .3841 .3999 .4695 .0196 .1884 1 .013 1 .012 1 .011 1 .008 1.022 1 .019
AO Rose Smoke .3557 .3833 .3992 .4689 . 0196 .1879 Medium 1. 011 1 .010 1 .009 1 .007 1.019 1.017
Noviol c .3542 .3820 .3980 .4678 .0194 .1868 1.008 1 .007 1 .006 1 .004 1 .012 1 .011
B & L. Smoke .3527 .3804 .3965 .4667 .0194 .1857 -No .' fr 1 .003 1.003 1 .002 1 .002 1 .008 1 .005
Cool Ray .3521 .3798 .3959 .4661 .019� .1851 blue/green 1. 001 1 .001 1 .001 1.000 1 .001 1 .002
No glass filter .3517 .3794 .3955 .4659 .0192 .1848
Polaroid Neutral .3509 . 3786 .3948 .4652 . 0191 .1842 .9977 .9979 .9981 .9987 .9962 .9966
I t--' V1 I
APPENDIX B2 LUMINOUS CONTRAST Illumination: Light Overcast
Elevation Conditions Rl-11 Rl-12 Rl-L3 R2 R3 R4
Wratten 23 11 y . 3685 .3958 .4109 .4786 .0208 .1978 Ratio # 2 1.049 1.044 1.040 1.028 1.081 1.072
Wratten 16 .3603 .3879 .4035 .4725 .0200 .1914 1.026 1. 023 1.021 1.015 1.042 1.037
Doc 2 .3591 .3866 .4023 .4714 .0199 .1905 1.022 1.020 1.018 1.013 1.037 1.033
Poloroid Yellow .3562 .3839 .3997 .4693 � 0196 - ·.:1882 1.014 1.013 1.011 1.008 1.022 1.020
AO Rose Smoke .3553 .3830 .3989 .4686 .0196 .1876 Medium 1.011 1.010 1.009 1.007 1.019 1.017
Noviol C .3541 .3817 .3977 .4676 .0194 .1866 1.008 1.007 1.006 1.005 1.012 1.011
B & L Smoke .3525 .3802 .3963 .4664 .0193 .1854 No 4 1.003 1.003 1.002 1.002 1.005 1.005
Cool Ray .3518 .3796 .3957 .4659 .0193 .1849 blue/green 1. 001 1.001 1.001 1. 001 1.003 1.002
No glass filter .3513 .3791 .3953 .4653 .0192 .1845
Poloroid Neutral .3506 .3783 .3945 .4649 .0191 .1339 .9979 .9981 .9982 .9888 .9964 .9969
I I-' (j\ I
APPENDIX C
�,_............._......_.,............- -....,.__,-- ..-....__,___ ...... ___ \ = �,
""'· 111tioi• I } ;
�fj I .• i
�oo - �' •20 oo aoo �·-o aeo 420 uo 100 No no eio .. o 990 WAV!\.U'tGllt fN Mtt.U�N$ 'r
FrnunE 17. Spectral lraiumiUances of@o•11 Smokt gla81M1. . -- � l\T.-1li11m Ro.•c 8mo1<1'.i 1-1.02 mm, Dstlt Rose Smo.:. �-,.1IO mn1, Amer!• rnn Optirnl Co. See ugtl{O 76 !or the epcetnll ID� trammlttanee ol Medium Role Smoke.
100 . -I i ·- P-1
50
ao
� �o � t: "40 . ' I a z .. 30 .. ..
20
10
0 ����-�-�-������WAVlL[HGlH IN Mff..LIMtQtOHS
Frnurui 18. Spectral trammiUancu of NOl!iot gla:111u. Novlol 0, t�2.63 lll.Il!t Noviot A, t-1.llo mm, Nol'iol B, t•2.811 mm, aud No.-iol C, t-3,0-5 mm, t;orolng Olaaa Works. ·
420 460 �oo � .. o "eo 620 660 · 100 7..-0 780 - ezo eso 900 WAVELEHGTff tH M1ll.1.M4C�0�5 FrauP.B 22. Spectral _tran_sm1·uance of Cool-Ray glas11; ·alsp the lumino:nty curv� of the eye •
• 1?0t·Rnyj t�l.92 mm, Amerirnn Optiml Co. The similarity of tbe S!Jt'eo •l1lcli ranCJ ttance curvee between Cool-Ray snd !>ther blu� glasses su s:i a obat, Ray·Ban., Wll.IJ<Jnlt&, etc., !3 mt.e=tlng. . -
Oiroulan of the N ationril Bnreav, of Standards
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-S!.wi<oNo.1 i-.:i.-o81iiw-;siiffiiioN•�.2; ,;_2;1J1mm�a;T-2.06 _1 mm nn<I 1-lrnokt1 No. 4, t�2.rn� mm, 111!!1-!idl & Lumb o·r� Co. Tllcso f �moko �h•'<"'S nro slmlw to ll11"'0 of'liifuro JI cxcxpl'"tor l1Ffur o"tiaelUcs In both lhu ullmvlolet nml. lnrtnrr.J SJM><>trnl rr� ""· 'l'hcsc �lll:!.•l"I aro nlw known 11.i No·ulml, NI, N2, N� uml N4. � f� llcuh1r IJ.llll!ltl!IDCll l""'nu.•u hf It• 1!.'l!l...Q.2'..
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!;; 60 .. u �� ! 401· tt %30 � i' � 20 ;'j �10
s�'O. MO- � 4t0 460 -600 &40 �IO 620 M-0 TOO 1� too 110 HO too-!) twAV!U:NO.fH Ut ... L\.i�
Frnunm 15. Spectral tranamitlcmce11 of Polarm'd olm1at<.•. � . J Nuutml Po!Jlrold, 1-�.20 mm, l'nll\folcl O!ly Ol11..,, 1-2.�m.JlDJ]..'l'.<4lnw Polo.rold, t-�.tJS lUnl. l'oliuohl Cur1l. 'l'hn !Hllrtplt1!1 t·on:-il�h·•l or polurh:fng filmj botwoen 11Jnt1·� of UJ,:ht l1Jul!<ih .. �rt·\•n g-lt\.tie!f, l\il ll�l of lltt" ,.,,lnr of th,, :<:un .. r.ll19 t\fl.J}(}lU':t lo bu <l.t.ll\"r1n,1wd by Uu..' 111U:ii'1U .. '1JI of a tlyy�wltblu tlt•' pnh\tb,11}{ uyor. �;_ ·.
'· . .-
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80
60
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400 lOll ibbilily: ill
DOC
18
23A
DOCLENS TRANSMISSION CURVE
�-4�� ���!--����--����-;-������. - ��-;;=--±-+ (2 _,. __ _
400 450 500 550 600 650 WAVELENGTH - rti\NO:M.ETE7.S
16 . ,I
IOll
29
700 1 '