36
AD-AlOI 056 ARNY ELECTRONICS RESEARCH AN DEVELOPMENT COMMAND VS--ETC PYR 20/6 BALENCE EFFECTS ON OPEN AtR MUL1IPATHS. tU '4 'R 1 R WATKINS, K 0 WHITE- L J CROW UNCLASSIFIED ERAAWiASL-TR-O086 EIIIIIIIIIIIl IIIIIIIIIIIIII EIIIIIIlIl

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Page 1: AD-AlOI ARNY ELECTRONICS RESEARCH AN DEVELOPMENT … · ad-aloi 056 arny electronics research an development command vs--etc pyr 20/6 balence effects on open atr mul1ipaths. tu '4

AD-AlOI 056 ARNY ELECTRONICS RESEARCH AN DEVELOPMENT COMMAND VS--ETC PYR 20/6BALENCE EFFECTS ON OPEN AtR MUL1IPATHS. tU '4

'R 1 R WATKINS, K 0 WHITE- L J CROWUNCLASSIFIED ERAAWiASL-TR-O086

EIIIIIIIIIIIlIIIIIIIIIIIIIIEIIIIIIlIl

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~IZI]

ASL-TR-0086 AD

\Reports Control Symbol

OSD-1366

.TURBULENCE EFFECTS ON OPEN AIR MULTIPATHS

0

~ MAY 1981

By

WENDELL R. WATKINSKENNETH 0. WHITELAURA J. CROW

Approved for public release; distribution unlimited

US Army Electronics Research and Development Command

S ATMOSPHERIC SCIENCES LABORATORYWhte Sarns Missile Rnge 7 NM 8802

t~ 706 011

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NOTICES

Disclaimers

The findings in this reoort are not to be construed as an officialJepartlflent of the Arimy position, unless so designated by otheratlhiurized documents.

Tqe citation of trade names and names of manufacturers in thisreport is not to be construed as official Government indorsementur approval of comimercial products or services referenced herein.

Disposition

Destroy this report when it is no longer needed. Do not return itto the originator.

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/1 / KSECURITY CLASSIFICATION OF THIS PAGE ("an Data Entered)

REPORT DOCUMENTATION PAGE BEFORE CNMPUET'R.MI. REPORT NUMBER 2. GOVT ACCESSION NO 3. RECIPIENT- CATALOG NJM-.rl

ASL-TR-0086 T-,' 101 )- , .

4. TITLE (id Subttle) S. TT!E OF REPORT 6 tiEre)1, UCVERED

TURBULENCE LFFECTS ON OPEN R D Final ReportAIR MULTIPATHS

6. PERFORMING ORG. REPOTRT NUMBER

'7. AUT-WdOL. . ... 8. CONTRACT OR GRANT NUMBER'*)

Wendell R.'Watkins, Kenneth O./White,Laura I] : Crow

9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. PROG M ELEMENT, PROJECT. TASKARE _AW ORK UNIT NUMBERS

,S Army Atmospheric Sciences Laboratory OA TA sk To.

White Sands Missile Range, NM 88002

I. CONTROLLING OFFICE NAME AND ADDRESS !2.-4GoRT DATE

US Army Electronics Research [- May 1.981(and Development Command 1 13. NJMBFP OF PAGES

5delnhi. MD20Z834 MO ITOIING AGENCY NAME & ADCRESS(lt differetf from Catrolling Office) 15. SECURITY CLASS. (of th h eport)

I, 1LASS IFIFn

15al OECL ASSI FIC ATION /D:OWN GPADIN GSCHEDULE

If DISTRIBU7ION STATEMENT (of thla Report)

Aprproved for public release; distribution unlimited.

;-7 DISTRIBUTION STATEMENT (of th abetract entered in Block 20, If dfferent from Report)

IA. SUPPL.EMENTARY NOTES

19. KEY WORDS (Continue on reaere side If necessary mid Identify by block number)

Open air multipathGas concentration monitorTurbulence

,20, A rR AC" rcmi tfve reWrse 04% tP rm,,memy ad Id"f*t by block nuinber)

'The possible effects of tu;-bulence on the maximum usable pathlength of an openair multipath were investigated. Open air multipaths can ,e used inconjunction with scanning optical sources to measure trace gaset along openair optical paths for Field testing of military electro-opti,.al systemsincluding high energy lasers. Turbulence was found to be the maj,- source ofsystem degradation for anl open air optical multipath. The effects ofturbulence on beam spreading as a function of position along the multipath

FORM M4 EDITION OF MC.. e I 1s OSOLETE 1

/ ,. 7 SECURITY CLASSIFICATION OF THIS PAGE (V- flata Rntered)

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SECURITY CLASSIFICATION OF THIS PAGE ren Dat. Entered

20. ABSTRACT (cont)

were measured. Multipath optics image and diffuse the input beam in a beamconserving fashion in producing the multipath. TLrbulence has its strongestdegrading effects on the diffused beams in the multipaths, thus open airmultipaths would require turbulence shielding of this portion of the opticalpath to be effectively used, especially during high daytime turbulencelevels. Such systems can, however, be easily used in enclosed buildingenvironments without any path shielding. _-

ST

i2

SECURITY CLASSIFICATION OF THIS PAGEr(17,.n Datel Entered)

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PREFACE

The authors acknowledge Donald L. Walters for his assistance in theexperimental setup and analysis of the turbulence measurements made duringthis investigation as well as his review of this report.

Aoession For

NTIS C7rA&IbTIC TAB

Diztribut ioi;/

Avai]..9a 111ty ds

Dist Scial

I. 3

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CONTENTS

INTRODUCTION ....... .............................. 7

EXPERIMENTAL APPROACH .................................................... 8

Measurements ............................ . ........................... 10

Measurement Results ............. .................................... 13

CONCLUSIONS .............................................................. 17

REFERENCES ............................................................... 1;

ffiECID1 PAC3 BANK-NOT FILMD

5

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INTRODUCTION

Atmospheric gases are major contributors to the degradation of high energylaser (HEL) beams and are significant contributors to the degradation ofelectro-optical (EO) systems. To compare test results with model predictionsfor such Army and Department of Defense systems, an accurate characterizationof the atmosphere during the testing is required; in particular, a measure isneeded of the concentrations of -he contributing gas species comprising theatmosphere. When one is concerneo with situations in which unknown gases maybe contributing to the absorption of the radiation, rapid identification ofthe gases and determination of their concentrations require use of techniquesinvolving a tunable spectral source, such as a Fourier transform spectrometer(FTS) or a diode laser. Spectrophone systems are not well suited for use withthe above spectral sources because they are low power sources and hencedegrade the spectrophone's sensitivity. One of the most sensitive means ofdetermining the gas species and concentrations is the use of tunable sourcesto scan absorption lines characteristic of the various gases. The energypropagates through a long optical path in a test environment such as the longfolded optical path produced by the White-type optics' of a multipathabsorption cell opened to the environment. There is, therefore, a need toinvestigate what the limits are on open air multipaths used in suchmeasurements.

At the Atmospheric Sciences Laboratory (ASL), White-type absorption cells havebeen used substantially and their operation has also been improved. -

6 Twofactors have been found to severely limit the maximum usable pathlengths. Oneis system vibration caused by ground movement, for example, from the proximityto vehicular traffic or winds which can cause the mirror mounts to sway. Thiseffect can be minimized if the mirrors are mounted relatively close to theground (1/2- to 1-m elevation at most). A second and more pronounced effectis that of temperature gradients along the path or equivalently, in the open

'John U. White, 1942, "Long Optical Paths of Large Aperture," J Opt Soc Am,32:285

2 Kenneth 0. White et al, 1978, "Water Vapor Continuum Absorption in the 3.5 -4.0 im Regions," Appl Opt, 17:2711

'Wendell R. Watkins et al, 1979, "Pressure Dependence of the Water VaporContinuum Absorption in the 3.5 - 4.0 um Region," Appl Opt, 18:111494

"Wendell R. Watkins et a!, 1979, "Water Vapor Absorption Coeff'cients at HFLaser Wavelengths (2.64 2.93 pm)," Appl Opt, 18:1582

sWendell R. Watkins, 1976, "Path Differencing: An Improvement to MultipassAbsorption Cell Measurements," Appl Opt, 15:16

'Wendell R. Watkins and Richard G. Dixon, 1979, "Automation of Long-PathAbsorption Cell Measuremcnts," Rev Sci Instrum, 50:86

7 B==1uG PniZ BL~mE-,Io FlZjaD

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air multipath, atmospheric turbulence. As a result, the effect of turbulence

on an open air multipath has been investigated by using White optics todetermine the feas~b 1l;ty of using such optics in a quasi-point gas sampler

capacity.

EXPERIMENTAL APPROACH

A set of 20-m White optics from an old longpath absorption cell greatlyfacilitated the 4nvestigation. The set of three spherically concave mirrcrscould easily be mounted (completely open to the laboratory environment) in the

end sections of the old 3b-orption cell. As a first crude assessment of hr .

well the absorpti,,n cell optics would work in an open air environment, inHe-Ne laser source was used with the White optics to produce a multiratO,

more than 1 km 25-sDot m,'toath). A pathlength of I km is - reaonaDestimate of the absorhing nath required to measure the speci,s a-.(concentrations of absorbirg gases which can significantly affect "'propagation of HEL and E3 system-. Details of how the multipaths are obta'.er

with White-type ortics are 21ven elsewhere. S, Under room air turh, ',edegradation of the outvit )eam was comparable in terms of beam epaiO.or3.litter, and wander to tn f]3riJation experienced in a sealed levacrab>

absoroDon c-11. Th-i wa'; indeed satisfying; for if a lonq cat',i ,nci'- ccoul'not be estab'ihed in a- enclosed room with low turbulence leve,, then itwould e 'mpossiblp to usp ')hp ' hite optics in a field environment.

Initially the plar wAs to deve'op and implement a scheme in the &bnOratory to,mnea,' p beam degradation an,_ turbulence level produced by an art "Wic4ai

turhu;Pnce sourcn -r1r then taKp t~le White optics outdoors and investiqate theeffects of open air turbu'ence on the multipath beam. For these tests av'sible He-Ne las-r was used even though most of the source wavelengths of

interpst are :- th, near infrared, The wavelength dependence of the turbulent

beam spread i s' qht, The results of the laboratory calibrationmeasurements wer- jch that only measurements of field turbulence levels wererequired to deterni-ne the effects on the multipath beam. Hence, the Whiteoptics did not nve to be taken to a field site.

The general setup for making measurements in the laboratory is shown in f4aure1. A 15-mW Spectr -Physics 124B He-Ne laser was used as the source. The

He-Ne beam was directed by using two flat mirrors so as to just miss thf edgeof the White optics' mirror M2 and be centered on mirror M1. Filters toad'ust the intensity of the beam as well as apertures to eliminate unwanted

Wendell R. Watkins, 1976, "Path Differencing: An Improvement to MultipassAbsorption Cell Measurements," Appl Opt, 15:16

'Wendell R. Watkins and Richard G. Dixon, 1979, "Automation of Long-PathAbsorption Cell Measurements," Rev Sci Instrum, 50:86

'D. L. Fried, 1966, "Limiting Resolution Looking Down Through the Atmosphere,"J Opt Soc Am, 56:1380

8

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POWERMETER

1 1Moved inanid out

CAMERA -- of Beam

He-Ne -------FILTER M3

M2

FM~ I I

Moved inAPERTURE -and out

of BeamFILTERF

He - Ne

LAERARTIFICIAL TURBULENCE

TURBULEN(E SENSORSOURCE

Figure 1. Experimental setup for measuring effects of optical turbulence onan open air multipath. An He-Ne laser was used and with ?,)-wWhite-type multipath cell mirrors M1, M2, and M3. The e-Ne inputbeam was tailored by using a filter, aperture, and flat mirrors. Acamera and p.wer fete- were used to monitor the He--'e outputbeam. Artificial turbulence could be introduced and murliLored inthe fnuLipath ;)eam.

9

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secondary beams were inserted in the beam before it entered the Whiteoptics. The three mirrors which comprise the White optics are sphericallyconcave with radius of curvature and separation distance of 20 m. Mirror MIdirects the beam to a position close to the edge of mirror M2. Mirror M2 thendirects the beam to the center of mirror M3. Finally, M3 either directs thebeam back to M2 or off the edge of M2 to form the output beam of themultipath. By rotating M3 about the axis normal to figure 1, the pathlengthcan be changed. The intensity of the output beam can then be monitored orphotographed to determine beam degradation caused by turbulence. --igure Ishows a top view of this He-Ne beam configuration throughout whi,-h the beam ioaoproximately 1/2 m above to'e laboratory floor.

Several sets of measurements were performed. First, the beam size wemonitored through time exposure photographs with ambient room tiurbul-:.,function of time of day. Next, an artificial heat source was moved ;,in"multipath to determine the jener,3l effects of high turoulence 'ev"'most pronounced effect occurred near mirrors MI and M3. A variac was used t'change the power level, and the -naximum pathlength (i.e., no beam c'op ",corresponding to a beam < 6 mm in diameter) was determined 'or ;evereturbulence levels. Concurrently for a fixed level of turbulence, ,-7 oercet.on the variac, the output beam size of a fixed 160-m multipath for a ,'; -

output intensity was ineasjred s a function of the positi-n o the t'b.'£oc"

source between mirror M2 and mirrors MI and M3. Finally, the zu ,len!eve7s n the laboratory, as well as outside under cloudy and clear con(-ti.tas a function of height above the ground, were measured.

Measurements

The measurement of the change in output beam size as a function of variations,n the room air turbulence throughout the day required a stobstantial amount ofi it4a! setup. Tl He-Ne 7ase- beam had to be adjusted oy using mirrors toenter the White optical syster,. The three 20-m White-type mirrors wererectangular (wlich does rot give the optimum configuration). The mirrors wereadjusted to give a multipath output for which the pathlength could be changedby rotating only mirror M3 as is described in detail elsewhere."' , A'ektronix C-12 oscilloscope camera with the lenses removed was used toonotograph the output beam. A narrow bandpass He-Ne filter was used toeliminate background light. Several tests were performed to determine anappropriate time exposure (5 s) and beam intensity which could be adjusted byinserting filters into the beam before the beam entered the White optics.Several problems were encountered in the system setup. To obtain a clearsinge-image output beam, the filters had to be tilted to diverge secondarybeam- away from the Drimary; and apertures were inserted to remove ghost

Wendell R. Watkins, 1976, "Path Differencing: An Improvement to MultipassAbsorption Cell Measurements," Appl Opt, 15:16

'Wendell R. Watkins and Richard G. Dixon, 1979, "Automation of Long-PathAbsorption Cell Measurements," Rev Sci Instrum, 50:86

10

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images before the bec;n entered the White optics. Tissue paper wa w"sertedinto the beam to obtain a diffuse speckle pattern for a ce l outrxt toprecisely align the camera and filtering system.

This setup was used iri photographing the output beam as a finction of time ofday. The beam size eid not noticeably change throughout the day or from dayto day, indicating that room air turbulence had little effect on the system.This finding was later verified by measuring the turbulence level in the

laboratory along the beam and throughout the day with a Cprobe descred

below. The laboratory turbulence was indeed low and stable, changing littlethroughout the day or along the White optics multipath as long as thelaboratory doors were closed and activity in the room was kept to a ,iinimum.After the technique for monitoring the change in size of the output )eam hadbeen developed, the effects of artificially induced turbulence wereinvestigated. A 125-W heat lamp was mounted in an insulated box .i.4 m on ,side. This arrangement produced a hot chimney which could be placed under themultipath anywhere between Lhe mirrors of the White-type optical system. Avariac was used to vary the artificial turbulence levels. The most pronouncedeffect of the artificial turbulence was seen when the source was situatedunder the multipath near the two-mirror-end of the White optics. To see howmuch effect the artificial turbulence had, the box was centered 1.44 m fromthe two mirrors and the variac setting was changed. The maximum usablepathlength was determined for each variac setting used. The tirbulencecorresponding to the various variac settings was then measured with a

calibrated probe (figure 2, obtained from Donald L. Walters of the ASI).

Basically the probe consists of two 3-W, 120-V light bulb filaments mounted 2('.cm apart on a rigid stand plus the associated electronics for obtaining anintegrated dc output voltage which corresponds to a measure of CT between the

probes. Complete details of the operation of the probes are giver

elsewhere." The amount of turbulence C2 present can easily be obtained fror:m

the values of CT or the output voltage. A calibration plot is given in figure3.

After the maximum pathlength was measured for a fixed location of theturbulence and for magnitude of the artificial turbulence source, the beamspread was measured for a fixed pathlength 160 m, for fixed turbilence level(45 percent on the variac), and for varying source positions along themultiuatl. Because this method of measurement required the comparison of

'Kenneth Kunkel et al, '79, "Atmospheric Conditions at the High Energy LaserSystem Test Facility (H.:.STF), White Sands Missile Range (WSMR). New Mexico,August 1977 to October 1178, Part I: Optical Turbulence, Wind, Temperature,Net Radiation, and Synoptic Weather Conditions," ASL-DR-79-(0,4, US ArmyAtmospheric Sciences Laboratory, White Sands Missile Range, NM

11

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A.1.14. IlllULB

211 M1 A VI I. mEN1'14

O"C I. A w11( )1

F

MI {j P1

yijuru, 3. Calibration curve fur the thermal probe AT sensor.

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photographs to determi:ie beam size, additional optics and instrumentation wereneeded. Two polarizing plates were used in the output beam to adjus the 'eamintensity. A power meter could be inserted into the beam to monitor the powerlevel. For each position of the artificial turbulence source, the polarizerswere rotated to obtain a constant He-Ne power output for each measurement.

Finally, the turbulence probe was taken outside to measure typical turb,,lencelevels during a hot sumimer day. The probe was used at 1/2- end 1-n elevationsand for clear and cloudy conditions.

Measurement Results

It was mentioned earlier that the White optics used were not the bestdesign. The mirrors were rectangular, which is especially bad for mirror M2(figure 1). The usual technique of getting the input and outpuit beams pastmirror M2 is to notch both sides of the upper half of the mirror, thusallowing the bottom row of images to start directly below the edge of theinput notch.' Use of a rectangular mirror for M2 required the first imagespot on M2 to be Positioned closer to the middle of the mirror than with anotched mirror. This positioning causes the maximum obtainable pathlengths tobe substantially reduced because the problem of clipping or mirror edges isenhanced. Thus some qualitative judgment had to be used in assessing whatdefined the maximum usable pathlength.

Clipping of the output beam was noted when the output beam diameter wasincreased due to the artificial turbulence by a little more than 50 oercentover the room air turbulence ri'meter. The maximum usable pathlength wasdefined as the longest pathlength for which beam clipping did not occur. Withthe artificial turbulence source centered 1.44 m from mirrors M1 and M3 andvariac settings of 15, 30, 45, 60, 75, and 90 percent, the maximum usablepathlength was determined. The results of these measurements are shown infigure 4. The CT probe was then used to determine the C2 turbulence level for

I Nthe variac settings. The output voltage of the CT probe was found to be quitelinear with variac setting (figure 5), having a 0.137-V offset corresponding

to C2 for room air turbulence of 8.7 x 10-15 m-2 /3. Note that t ;e input beamNwas 4 mm in diameter and spherically diverged to about 2.0 cm over the 20 mbetween M2 and mirrors 4I and M3. Mirrors M1 and M3 focused the oeam to 4 mmunder room air turbulence.

The next step in assess'ig how turbulence affects the multipath formed by theopen air White optics wa; to fix the pathlength at 160 m (or eit' t traversalsbetween the mirrors), fix the artificial turbulence level at 45 percent or a

value of C2 of 3.5 x 1I - 12 m-21 3, and vary the location of '.e turbulenceN

'Wendell R. Watkins, 1976, "Path Differencing: An Improvement to MultipassAbsorption Cell Measureints," Appl Opt, 15:16

13

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[-q 640

t80

320

. 160

* , I

0 30 60 90

% OF LAMP HEATFigure 4. Maximum Dathlength as a Function of increased artificial turbulence

at the two-mirror-end t tne multipath.

0. 10 2) :0 10 50

VARIA(' SETTING(

Pigure 5. Linearity of turbulence level in the multipath in terms of probeoutput voltage with respect to artificial source turbulence interms of varlac power setting.

14

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sourbe along the m.: tipath to determine the functiona! de)endence ofturbulence location or, amount of beam spread. As described earlier, this stppwas accomplished by cemparing 5-s exposure photographs of the He.Ne heam. Apair of polarizers we- placed in the output beam; and for each tirbulenc -location, the polarizets were rotated to give a total cell output Dower of 0.4mW. Photographs were then taken with the power meter removed, and the beo'ndianeter was measured :y averaging the width and height of the central maxinu.of the beam since ,he beam was slightly irregular i.1 shape on thephotographs. The average of three data runs for ten path locations for theturbulence source is shown as circles in figure 6 with the soii. cwj;-verepresenting an eyeball fit to the data. The figure shows subst.ntiallv -norebean spreading as the turbulence is moved closer to the double mirror end o'the multipath. Some of this spreading dependence can be accounted for by thefact that the beam is spherically diverging between mirror M2 and rnrrors M!,id M3.

The final measurement was to determine turbulence levels in the realatmosphere. Measuremerts had already been made for high summer turbulencelevels at 5-m and 32-m elevations as shown in figure 7. At midday

the C 2 turbulence leve! reaches 10- !4 m-2/3 for 32 m and 10- 13 m "2/3 for 5-,N

elevation. Further measurements were needed for this study since the Whiteoptics can be situated between only 1/2 and 1 m above the ground witho:tcausing serious vibrations problems. Consequently, the C2 temperature probe

Twas taken outdoors to obtain values corresponding to midday turbulence levelsFor clear and clonudy :,nditions at 1,2- and 1-m elevations. The meas::reenlresults are shown in rdble 1.

An atte-npt was made to calculate the maximum usable pathlength as d functionof turbulence leveis, but this approach presented some very serioustheoretical problems, and it becdme clear that to obtain solutions to theseproblems (if possible) was completely beyond the scope of this work effort.Therefore, no theoretical discussion will be given. In the conclusions whichfollow, insight gaino' during the attempt at analytical understanding isincluded.

15

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5.0)

/

1.5/

,,IS 13 24)

I1,' \4 'i: FROM SIN(;E MIRROR m i

Figure 6. Functiona' dependence of the effects of output beam spread in termsof beam dameter -d location of artificial turbulence source alongthe 160-m nultipath as measured from the single-mirror-end.

20 JUNE 1976 CLOUDS PARTLY CLOUDY

- 4. . . . . ( . .t .

- A

i "16

I METERSC 2 . ME1TERS

2 1 4 4 1 111 1$ I 1 Is 20 22 2

HOURS ( MST)

Figure 7. Hourly thermal turbulence measurements of C2I at WSMR for elevations

of 5 m (triangles) and 32 m (squares). Data obtained from Glenn B.Hoidale et al, "Micro-Meteorological Measurements forElectro-Optical Propagation Tests at White Sands Missile Range,"Pr2ceeding of the 'ptica l-Submillimeter Atmospheric PropagationConference. , 6-9 December 1976.

16

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TABLE 1. TYPICAL OUTDOOR TURBULENCE LEVELS MEASURED AT WSMR

Sky Conditions Elevation (m) Average C2N

Clear 1/2 1.3 x 10-12

Clear 1 7.3 x 10-13

Cloudy 1/2 1.3 x 10- 13

Cloudy 1 5.7 x 10- 14

CONCLUSIONS

The present investigation has provided much insight into the peculiarities ofthe White optics multipath. From the data shown one can see that real-worldatmospheric turbulence levels are comparable to those levels artificiallyinduced in the laboratory. Usable pathlengths will thus be less than 500 munder clear sky conditions; hence, such a system would not be particularlyuseful. Although White-type optics cannot simply be taken to a field site andused with an FTS or diode laser to measure gas concentrations and species,they can be employed under enclosed experimental conditions such as a largebuilding. For the first time, the weighting function of turbulence on beamspread as a function of position between the end mirror has been measured(figure 6). Sufficient experimental data could not be obtained within thealloted time frame to feasibly define the functional dependencies; however,enough definition was obtained to establish that, without shielding the two-mirror-end of the multipath, the nominal open air turbulence level so severelydegrades the maximum usable pathlength that the measurement scheme will notwork. Fortunately, the measurements also lead to a possible solAtion to theproblem because the effects of shielding the two-mirror-end of the multipathcould be assessed without extensive field measurements. Shielding the last 3m of the 20-m optical system used appears to be sufficient to allow akilometer usable multipath to be established even during the high middayturbulence on clear summer days at White Sands Missile Range.

17

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REFERENCES

I. White, John U., 1942, "Long Optical Paths of Large Aperture," J Opt SocAm, 32:285.

2. White, Kenneth 0., et al, 1978, "Water Vapor Continuum Absorption in the3.5-4.0 .m Region," Appl Opt, 17:2711.

3. Watkins, Wendell R., et al, 1979, "Pressure Dependence of the Water VaporContinuum Absorption in the 3.5 - 4.0 v-m Region," Appl Opt, 18:1149.

4. Watkins, Wendell R., et al, 1979, "Water Vapor Absorption Coefficients atHF Laser Wavelengths (2.6d - 2.93 m)," App) Opt, 18:1582.

5. Watkins, Wendell P., 1976, "Path Differencing: An Imorovement iL

Multipass Absorption Cell Measurements," Appl Opt, 15:16.

6. Watkins, Wendell R., and Richard G. Dixon, 1979, "Automation of Long-pathAbsorption Cell Measurements," Rev Sci Instrum, 50:86.

7. Fried, D. L., 1966, "Limiting Resolution Looking Down Through theAtmosphere," J Opt Soc Am, 56:1380.

8. Kunkel, Kenneth, et al, 1979, "Atmospheric Conditions at the High EnergyLaser System Test Facility (HELSTF) White Sands Missile Range (WSMR), NewMexico, August 1977 to October 1978, Part I: Optical Turbulence, Wind,Temperature, Net Radiation, and Synoptic Weather Conditions," ASL-DR-79-0004,US Army Atmospheric Sciences Laboratory, White Sands Missile Range, NM.

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DISTRIBUTION LIST

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National Center for Atmos Rsch Mil Asst for Atmos Sci Ofc ofMesa Library the Undersecretary of DefenseP. 0. Box 3000 for Rsch & Engr/E&LS - RM 3D129Boulder, CO 80307 The Pentagon

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AFATL/DLODLHugh W. Albers (Executive Secretary) Technical LibraryCAO Subcommittee on Atmos Ps:h Eglin AFB, FL 32542National Science Foundation Room 510Washington, DC 2055 Naval Training Equipment Center

ATTN: Technical Infcrmation ,Dr. Eugene W. Bierly Orlando, FL 32813Director, Division of Atmos SciencesNational Scinece Foundation Technical Library1800 G Street, N.W. Chemical Systems LaboratoryWashington, DC 20550 Aberdeen Proving Ground, MD 21010

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Chief CommanderIntel Mat Dev & Spt Ofc ERADCOM Scientific AdvisorAITN: DELEW-WL-I ATTN: DRDEL-SABldg 4554 Fort Monmouth, NJ 077C3Fort George G. Mead, MD 20755 Commander

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ATMOSPHERIC SCIENCES RESEARCH REPORTS

1. Lindberg, J. D. "An Improvement to a Method for Measuring the AbsorptionCoefficient of Atmospheric Dust and other Strongly AbsorbinqPowders," ECOM-5565, July 1975.

2. Avara, Elton P., "Mesoscale Wind Shears Derived from Thermal Winds,"ECOM-5566, July 1975.

3. Gomez, Richard B., and Joseph H. Pierluissi, "Incomplete Gamma FunctionApproximation for King's Strong-Line Transmittance M'odel,ECOM-5567, July 1975.

4. Blanco, A. J., and B. F. Engebos, "Ballistic Wind Weighting Functions forTank Projectiles,' ECOM-5568, August 1975.

5. Taylor, Fredrick J., Jack Smith, and Thomas H. Pries, "CrosswindMeasurements through Pattern Recognition Techniques," ECOM-5569.July 1975.

6. Walters, D. L., "Crosswind Weighting Functions for Direct-FireProjectiles," ECOM-5570, August 1975.

7. Duncan, Louis D., "An Improved Algorithm for the Iterated MinimalInformation Solution for Remote Sounding of Temperature," COM-5571,August 1975.

8. Robbiani, Raymond L., "Tactical Field Demonstration of Mobile WeatherRadar Set AN/TPS-41 at Fort Rucker, Alabama," ECOM-5572, August1975.

9. Miers, B., G. Blackman, D. Langer, and N. Lorimier, "Analysis of SMS/GOESFilm Data," ECOM-5573, September 1975.

10. Manquero, Carlos, Louis Duncan, and Rufus Bruce, "An Indication fromSatellite Measurements of Atmospheric CO2 Variability." ECOM-5574,September 1975.

11. Petracca, Carmine, and James D. Lindberg, "Installation and Operation ofan Atmospheric Particulate Collector," ECOM-5575, Septenber 1975.

12. Avara, Elton P., and George Alexander, "Empirical Investigation of ThreeIterative Methods for Inverting the Radiative Transfer Equation,"ECOM-5576, October 1975.

13. Alexander, George D., "A Digital Data Acquisition Interface for the SMSDirect Readov., Ground Station - Concept and Preliminary Design,"ECOM-5577, October 1975.

14. Cantor, Israel, "Enhancement of Point Source Thermal Radiat on UnderClouds in a Noiattenuating Medium," ECOM-5578, Octobey 975.

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15. Norton, Colburn, and Glenn Hoidale, "The Diurnal Variation of MixingHeight by Month over White Sands Missile Range, NM," ECOM-5579,November 1975.

16. Avara, Elton P., "On the Spectrum Analysis of Binary Data," ECOM-5580,November 1975.

17. Taylor, Fredrick J., Thomas H. Pries, and Chao-Huan Huang, "Optimal WindVelocity Estimation," ECOM-5581, December 1975.

13. Avara, Elton P., "Some Effects of Autocorrelated and Cross-CorrelatedNoise on the Analysis of Variance," ECOM-5582, December 197.

19. Gillespie, Patti S., R. L. Armstrong, and Kenneth 0. White, "The 2 ectrcZ

Characteristics and tmospheric CO, Absorption of the Ho+ 3 :v'Y 'ase-at 2.05,m," ECOM-55 3, December 1975.

20. Novlan, David J., "Ar Empir'cal Method of Forecasting Thunder .2v 'orthe White Sands Miss:!- Range," ECOM-5584, cebrijary 1976.

21. Avara, Elton P., "Randomization Effects in Hypothesis Testing withAutocorrelated Noise," ECOM-5585, February 1976.

22. Watkins, Wendell R., "Improvements in Long Path Absorption CellMeasurement," ECOM-'5)r6, Mirch 1976.

23. Thomas, Joe, George D. Alexander, and Marvin Dubbin, "SATTEL - An ArmyDedicated Meteorological Telemetry System," ECOM-5587, March 1976.

24. Kennedy, 5ruce W., and Delbert Bynum, "Army User Test Program for thePD7&-X1-75 Meteorological Rocket," ECOM-5588, April 1976.

25. Bdrnett, Kenneth M., "A Description of the Artillery MeteorologicalComparisons at White Sands Missile Range, October 1974 - December1974 ('PASS' - Prototype Artillery [Meteorological] Subsystem),"ECOM-5589, April 1976.

26. Miller, Walter B., "Preliminary Analysis of Fall-of-Shot From Project'PASS'," ECOM-5590, A ,ril 1976.

27. Avara, Elton P., "Error Analysis of Minimum Information and Smith'sDirect Methods for Inverting the Radiative Transfer Equation,"ECOM-5591, April 1976.

28. Yee, Young P., James D. Horn, and George Alexander, "Synoptic ThermalWind Calculations from Radiosonde Observations Over the SouthwesternUnited States," ECOM-5592, May 1976.

24

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29. Duncan, Louis [)D., and Mary Ann Seagraves, "Applications of EmpiriralCorrection. to NOAA-4 VTPR Observations," ECOM-5593, Mey .

30. Miers, Bruce T. and Steve Weaver, "ADplications of MeteoroogicalSatellite F ata to Weather Sensitive Army Operatios," FCOM-5594, M:1976.

31. Sharenow, Moses "Redesign and Improvement of Balloon 11L-966," ECOM-559'June 1976.

3). "ansen, Frank '., 'The Depth pf the Surface Boundary L ;yer," ECOM-5596,June 1976.

33. Pinnick, R. G., and E. B. Stenmark, "Response Calculations for aCommerica' '-ight-Scittering Aerosol (ounter," [COM-5597, July 1976

34. Mason, J., ano I. B. Hoidale, "Visibility as an Estimator of InfraredTransmittaricp," £COM-5598, July 1976.

35. Bruce, Pufus E.. Lous D. Duncan, and Joseph H. Pierluissi, "Experiment ,Study of the Relationsoip Between Radiosonde emperatures artRadiometric-Area Temperatures," ECOM-5599, August 1976.

36. Duncan, Louis 3., "Stratospheric Wind Shear Computed from SatelliteThermal Sounder Measurements," ECOM-5800, September 1976.

37. Taylor, F., P. Mohan, P. Joseoh, and T. Pries, "An All Digital AutoriateWind Measurement System," ECOM-5 801, Sentember 1976.

33. Bruce, Ch~rles, "Development of Spectrophones for CW and Dulsed RadiaticSources," ECOM-5802, September 1976.

39. Duncan, Louis D., and Mary Ann Seagraves, "Another Method for Estimatin,Clear Column Radiances," ECOM-5803, October 1976.

4(. ?lanco, Abel ,;. trid Larry E. Taylor, "Artillery Meteoroloncal Analysiof Project Pass," ECOM-5804, October 1976.

41. Miller, Walter, and Bernard Engebos, "A Mathematical Structire forRefinement o Sound Ranging Estimates," ECOM-5805, November 1976.

42. Gillespie, James B.. and James D. Lindberg, "A Method to Obtain DiffuseReflectance "easurements from 1.0 and 3.Oum Usin." a Cary 171Spectrophoto-;oter," ECOM-5806, November 1976.

43. Rubio, Roberto, ar Robert 0. Olsen, "A Study of the Effec.- ofTemperature 'ariations on Radio Wave Absorptiori" ECOM-5807,November 1976.

25

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44. Ba~lar', Harold N., "emperiture Measurements in the Stratosphere fromR a oon-Borne T nst-'ument Platforms, 1969-1915," ECOM-5808, Decemher197o.

45. Monahan, H. H., "An Approach to the Short-Range 0rediction of Early

Morning Radiation Foa,' ECOM-5809, January 1977.

4'. Engebos, Bernard Francis, "Introduction to Multiple State Multiple Action,Iecisron Theory and Tt, Relation to Mix<na Structu-ec," FCr)M-5Plr,

" .w. 5-chard . . , " of Cloid 'articles on Remo t e Sensnc~ 7 ,- '

Sp)ace th- :) - Y - -eter !nfrared _, , r-ror," 7M.K - , " 7

4' . Bonner, Pobert ., and ?. Nowton, "Appl ication of the A/GVS-5 LaserRaenqe~'nder v o -.< e He int Meas.rnments, K"-C-I2, " hc,.197'.

49. Rubio, Roberto, "L'd .tecion of Subvisihle eentry Vehicle lruvs'I'tdosnn Md*e A, COM-5813, Marcr IQ7.

,C. Low, Richard .. H., and .. Horn, "Mesoscale Determinatioi ol 'Cloud-Height: aroblems ind 'olutions," ECWM-5314, March 1977.

51. Duncan, Louis U., and Mary nn Seagraves, "Evaluation ,& the NOAA-4 V-D7,

Thermal W4nos for N'jclear Fallout Predictions," ECOM-5815, '4arc!.1917.

52. Randhawa, Ja'ur S., M. lzquierdo, Carlos McDonald, and Zvi Salpete-,.Stratosaneic "zone Density as Measured by a Chemilutrinescent

Censor 7,r g the Stratcom VI-A Flight," ECOV-5816, ADri, 1977.

53. R-bio, Roberto, and 'Aike Izquierdo, "Measurements of Net Atmospheric'rradiance in the C.7- to 2.8-Micrometer Infrared Region,"

ECOM-5iII, May 1977.

54. Ballard, Harold N., Jose M. Serna, and Frank P. Hudson, Consultant for(Themica ! "onetics, "Calculation of Selected Atmospheric Compositionr"aramet ers for the Mid-Latitude, September Stratosphere," ECOM-5918,

May 197'.

55. vitchell, J. 0., R. S. Sagar, and R. 0. Olsen, "Positive Ions in theMiddle At~nosphere During Sunrise Conditions," ECOM-5819, May 1977.

5b. White, Kenneth 0., Wendell R. Watkins, Stuart A. Schleusener, and RonaldL. Johnson, "Solid-State Laser Wavelength Identification Using aReference Absorber," ECOM-5820, June 1977.

57. Watkins, Wendell R., and Richard G. Dixon, "Automation of Long-PathAbsorption Cell Measurements," ECOM-5821, June 1977.

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58. Taylor, S. E., . M. Davis, and J. B. Mason, "Analysis of Observe.! Soi'Skin Moisto,-e Effects on Reflectance," FCOM-5822, lune 197'.

59. Duncan, Louis D., and Mary Ann Seagraves, "Fallout Predictio.ns Computedfrom Satell te Derived Winds," ECOM-5823, June 1977.

60. Snider, D. E., r G. Murcray, F. H. Murcray, and W. J. Williams,":.nvestigati on of High-Altitude inhanced Infrared 9ackrour,.Emissions," (U), SECRET, ECOM-5824, June 1977.

61. Dubbir, Mar'.,in 'I., and Dennis Hall, "Synchronous Meteorologca! %atellit-Direct ,dout Ground System Digital Video Flectronirs," ECr M-:)825,June 1977.

62. Miller, W.. ano F. 1ngebos, "A Preliminary Analysis of Two Sound RangingAlgorithws, EC.OM-5826, July 1977.

63. Kennedy, Bruce W., and James K. Luers, "Ballistic Sphere Techniques forMeasoring A'nmospneric Parameters," ECOM-5827, July 1977.

64. Duncan, Louis D., "Zenith Angle Variation of Satellite Thermal SounderMeasurements," ECOM-5823, August 1977.

65. Hansen, Frank V., "The Critical Richardson Number," ECOM-5829, September1(77.

t6. Ballar.4 Harold N., and Frank P. Hudson (Compilers), "Stratospheric.'pusitio;n Balloon-Borne Experiment," .C9M-5830, October 1977.

-7. 3ar'. W: Ia, C., and Arnold C. Peterson, "W'nd Measuring Accuracy Testof ',Wteo".W!oqical Systems," ECON-5831, '%'ember 1977.

b8. Hr .e, G. A., and F. V. Hansen, "Atmrip ,eric Diffusion: Similarityr"7ejv n~d Fmoirical Derivitions or Usp in Boundary Laver Diffusio",

69. Low, Ri, aard D. 0., "The !nternal Cloud Radiation Field and a Technique

for Determii;nq Cloud Riackiiess," ECOM-5833, December 3977.

Aat ,, v'en_ , Kenneth 0. White, Charles W. Bruce, Dondld L.

W: ters, -.nI J3,nes D. Lindberg, "Measurements Required forPrediction o- High Energy laser Transmission," ECOM- r334, December• 977.

71. Rrbio, kobert, "Investigation of Abrupt Decreases in Atmos!,'ericallyBac&scattered .aser Energy," ECOM-5835, December 1977.

72. r.nahan, H. H., and R. M. Cionco, "An Interpretative Review of ExistingCapabilities for Measuring and Forecasting Sel ,! 'ted WeatherVariables (Er.riasizing Remote Means),' ASL-TR-O001, J.i*uary 1978.

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73. Heaps, Melvin G., "The 1979 Solar Eclipse and Validation of D-RegionModels," ASL-TR-0002, March 1978.

74. Jennings, S. G., and J. B. Gillespie, "M.I.E. Theory Sensitivity Studies- The Effects of Aerosol Complex Refractive Index and SizeDistribution Variations on Extinction and Absorption Coefficients,Part IT: Analysis of the Computational Results," ASL-TR-0003, March1978.

75. White, Kenneth 0., et al, "Water Vapor Continuum Absorption in the. .5to 4.0gm Region," ASI-T-0004, March 19,8.

76. Oison, Robert 0., and B'ruce 1. Kennedy, "ABRES Pretest AtmosoherMeasurements,' PS_-Tk-PO'5, AprIl 1978.

77. Ballard, Harold N., ,ose '. Serna, and Frank P. Hudson, "Calcu'at]n J-Atmospheric Cc):-wos,, on in the High Latitude Se te '.e-Stratosphere," ASL-Q-I906, May 1978.

78. Watkins, Wendell R., et a , "Water Vapor Absorption Coefficients :t '

Laser Wavelengths," ASL-TR-0007, May 1973.

79. Hansen, Frank V., "Te Growth and Prediction of Nocturnal Inversions,"ASL-TR-0008, May 1973.

80. Samuel, Christine, Charles Bruce, and Ralph Brewer, "SpectrophoneAnalysis of Gas Samples Obtained at Field Site," ASL-TR-000q, June1978.

81. Dinnick, R. G., et al., "Vertical Structure in Atmospheric Fog and Hazeand its Effects on IR ×xtinction," ASL-TR-O010, July 1978.

32. Low, Richard D. H., Louis D. Duncan, and Richard B. Gomez, "TheMicrophysical Basis of Fog Optical Characterization," ASL-TR-O011,August 1978.

83. Heaps, Melvin G., "The Effect of a Solar Proton Event on the MinorNeutral Constituents of the Summer Polar Mesosphere," ASL-TR-0012,August 1978.

84. Mason, James B., "Light Attenuation in Falling Snow," ASL-TR-0013, August1978.

35. Blanco, Abel J., "Long-Range Artillery Sound Ranging: 'PASS' Meteorolog-ical Application," ASL-TR-0014, September 1978.

86. Heaps, M. G., and F. E. Niles, "Modeling of Ion Chemistry of theD-Region: A Case Study Based Upon the 1966 Total Solar Eclipse,"ASL-TR-O015, September 1978.

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87. Jennings, S. G., and R. G. Pinnick, "Effects of Particulate ComplexRefractive Index and Particle Size Distribution Variations onAtmospheric Extinction and Absorption for Visible ThroughMiddle-lnfr~red Wavelengths," ASL-TR-0016, September 1978.

88. Watkins, Wendell R., Kenneth 0. White, Lanny R. Bower, and Brian Z.Sojka, "Pressure Dependence of the Water Vapor Continuum Absorptiorin the 3.5- to 4.0-Micrometer Region," ASL-TR-0017, September 1978.

89. Miller, W. B., and B. F. Engebos, "Behavior of Four Sound RangingTechniques in an Idealized Physical Environment," ASL-TR-0018.Septembe- 1978.

90. Gomez, Richard G., "Effectiveness Studies of the CBU-88/B Bomb, Cluster,Smoke Weapcn," (Ii), CONFIDENTIAL ASL-TR-0019, September 1978.

91. Miller, August, Richard C. Shirkey, and Mary Ann Seagraves, "Calculationof Thermal Emission from Aerosols Using the Doubling Technique,"ASL-TR-0020, November 1978.

92. Lindberg, James D., et al, "Measured Effects of Battlefield Dust andSmoke on Visible, Infrared, and Millimeter WavelengthsPropagation: A Preliminary Report on Dusty Infrared Test-!(DIRT-I)," ASL-TR-0021, January 1979.

93. Kennedy, Bruce W., Arthur Kinghorn, and B. R. Hixon, "Engineering FlightTests of Range Meteorological Sounding System Radiosonde,'ASL-TR-0022, February 1979.

94. Rubio, Roberto, and Don Hoock, "Microwave Effective Earth Radius FactorVariability at Wiesbaden and Balboa," ASL-TR-0023, February 1979.

95. Low, Richard D. H., "A Theoretical Investigation of Cloud/Fog OpticalProperties and Their Spectral Correlations, "ASL-TR-0024, February1979.

96. Pinnick, R. G., and H. J. Auvermann, "Response Characteristics ofKnollenberg Light-Scattering Aerosol Counters," ASL-TR-0025,February 1979.

97. Heaps, Melvin G., Robert 0. Olsen, and Warren W. Berning, "Solar Eclipse1979, Atmospheric Sciences Laboratory Program Overview,"ASL-TR-0026, February 1979.

98. Blanco, Abel J., "Long-Range Artillery Sound Ranging: 'PASS' GR-8 SoundRanging Data," ASL-TR-0027, March 1979.

99. Kennedy, Bruce W., ind Jose M. Serna, "Meteorological Rocket NetworkSystem Reliability," ASL-TR-0028, March 1979.

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100. Swingle, Donald M., "Effects of Arrival Time Errors in Weighted RangeEquation Solutions for Linear Base Sound Ranging," ASL-TR-0029,April 1979.

101. 'Jmstead, Robert K., Ricardo Pena, and Frank V. Hansen, "KWIK: AnAlgorithm for Calculating Munition Expenditures for SmokeScreening/Obscuration in Tactical Situations," ASL-TR-0030, Aprfl1979.

102. D'Arcy, Edward M., "Accuracy Validation of the Modified Nike HerculesRadar," ASL-TR-0031, May 1979.

103. Rodriguez, Ruben, "Evaluation of the Passive Remote Crosswind Seiso-,ASL-TR-0032, May 1979.

104. Barber, T. L., and R. Rodr 4guez, "Transit Time Lidar Measurement -

Near-Surface Winds in toe Atmosphere," ASL-TR-0033, May 1972.

105. Low, Richard D. P., Louis D. Duncan, and Y. Y. Roger R. Hsiao, "Micro-physical and Optical Properties of California Coastal Fogs V crOrd," ASL-TR-0034, June 1979.

106. Rodriguez, Puben, and William J. Vechione, "Evaluation of the SitjratiorResistant Crosswind Sensnr," ASL-TR-0035, July 1979.

107. Ohmstede, William D., "The Dynamics of Material Layers," ASL-TR-0036,July 197Q.

108. Pinnick, R. G., S. G. Jennings, Petr Chylek, and H. J. Auvermann,"Relationships between IR Extinction Absorption, and Liquid WaterContent of Fogs," ASL-TR-0037, August 1979.

109. Rodriguez, Ruben, and William J. Vechione, "Performance Evaluation ofthe Optical Crosswind Profiler," ASL-TR-0038, August 1979.

110. Miers, Bruce T., "Precipitation Estimation Using Satellite Data,"ASL-TR-0039, September 1979.

111. Dickson, David H., and Charles M. Sonnenschein, "Helicopter Remote WindSensor System Description," ASL-TR-0040, September 1979.

112. Heaps, Melvin G., and Joseph M. Heimerl, "Validation of the DairchemCode, I: Quiet Midlatitude Conditions," ASL-TR-O041, September1979.

113. Bonner, Robert S., and William J. Lentz, "The Visoceilometer: APortable Cloud Height and Visibility Indicator," ASL-TR-0042,October 1979.

114. Cohn, Stephen L., "The Role of Atmospheric Sulfates in BattlefieldObscurations," ASL-TR-0043, October 1979.

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115. Fawbush, E. J., et al, "Characterization of Atmospheric Conditions atthe High Energy Laser System Test Facility (HESTF), White SandMissile Ra-ge, New Mexico, Part 1, 24 March to 8 April 1977,"ASL-TR-O044, November 1979.

116. Barber, Ted L., "Short-Time Mass Variation in Natural Atmospheric Du~t,ASL-TR-0045 November 1979.

117. LOW, Richard D. H., "Fog Evolution in the Visible and Infrared SpectralRegions and its Meaning in Optical Modeling," ASL-TR-0O46, December1979.

118. Duncan, Louis D., et al, "The Electro-Optical Systems AtmosphericEffects Library, Volume 1: Technical 0ocumentation," ASL-TR-O04;December 1979.

119. Shirkey, R. C., et al, "Interim E-O SAEL, Volume II, Users Manual,"ASL-TR-O048, December 1979.

120. Kobayashi, H. K., "Atmospheric Effects on Millimeter Radio Waves,'ASL-TR-0049, January 1980.

121. Seagraves, Mary Ann, and Louis D. Duncan, "An Analysis of Transmittance;Measured Through Battlefield Dust Clouds," ASL-TR-0050, February1980.

122. Dickson, David H., and Jon E. Ottesen, "Helicopter Remote Wind SensorFlight Test," ASL-TR-0051, February 1980.

123. Pinnick, R. G., and S. G. Jennings, "Relationships Between RadiativeProperties and Mass Content of Phosphoric Acid, HC, Petroleum Oil,and Sulfuric Acid Military Smokes," ASL-TR-0052, April 1980.

124. Hiids, B. 0., and J. B. Gillespie, "Optical Characterization ofAtmospheric Particulates on San Nicolas Island, California,'ASL-TR-0053, April 1980.

125. Miers, Bruce T., "Precipitation Estimation for Military Hydroloqy,"ASL-TR-0054, April 1980.

126. Stenmark, Ernest R., "Objective Quality Control of Artillery ComputerMeteorologicai Messages," ASL-TR-0055, April 1980.

127. Duncan, Louis D., and Richard D. H. Low, "Bimodal Size DistributionModels for Fols at Meppen, Germany," ASL-TR-0056, Aprii 1980.

128. Olsen, Robert 0., and Jagir S. Randhawa, "The Influence of AtmosphericDynamics on Oz.one and Temperature Structure," ASL-TR-0057, May 1980.

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129. Kennedy, Bruce W., et al, "Dusty Infrared Test-11 (DIRT-Il) Program,"ASL-TR-0058, May 1980.

130. Heaps, Melvin G., Robert 0. Olsen, Warren Berning, John Cross, andArthur Gilcrease, "1979 Solar Eclipse, Part I - Atmospheric SciencesLaboratory rield Program Summary," ASL-TR-0059, May 1980

131. Miller, Walter B., "User's Guide for Passive Target Acquisition Prograf-Two (PTAP-2)," ASI,-TR-060, June 1980.

132. Holt, E. H., editor, "Atmosiheric Data Requiremren's or Bttle'&dObscuration Applicatinons," ASL-TR-0O61, June !8Q.

133. Shirkey, Richard C., Mjist Miller, George 4. T,)ed-cke, o, d VjC, " ,'"Single Scattering, Code AGAUSX: Theory, Applications, Comp sn .and Listing," ASL-TP-!06?, July 1980.

134. Sojka, Brian Z., and Kernet" 0. White, "Evaliation of SpecializedPhotoacoustic Absor-tion Chambers for Near-Mi~limeter Wave (NMMV!Propagation Measurements," ASL-TP-0063, August 1980.

135. Bruce, Charles W., Young Piul Yee, and S. C. Jennings, 'n S'tuMeasurement of t'e 'atio of Aerosol Absorption to Extinct ,.Coefficient," ASL-TR-0J64, August 19'00.

136. Yee, Young Paul, Charles W. Bruce, and Ralph J. Brewer,"Gaseous/Particulate Absorption Studies at WSM using Laser SourcedSpectrophones," AS-TP-0065, June 1980.

137. Lindberg, James 0., Radon B. Loveland, Melvin Heaps, James b. Gillespie,and Andrew F. Lewis, "Battlefield Dust and AtmosphericCharacterization Measurements During West German SummertimeConditions in Support of Grafenwohr Tests," ASL-TR-0066, Septenbcr1980.

138. Vechione, W. J., "Evaluation of the Environmental Instruments,Incorporated Series 200 Dual Component Wind Set," ASL-TR-0067,September 1980.

139. Bruce, C. W., Y. P. Yee, B. D. Hinds, R. G. Pinnick, R. J. Brewer, andJ. Minjares, "Initial Field Measurements of Atmospheric Absorptionat 9om to llpm Wavelengths," ASL-TR-0068, October 1980.

140. Heaps, M. G., R. 0. Olsen, K. D. Baker, 0. A, Burt, L. C. Howlett, L, L.Jensen, E. F. Pound, and G. D. Allred, "1979 Solar Eclipse: Part IIInitial Results for Ionization Sources, Electron Density, and MinorNeutral Constituents," ASL-TR-0069, October 1980.

141. Low, Richard D. H., "One-Dimensional Cloud Microphysical Models forCentral Europe and their Optical Properties," ASL-TR-0070, October1980.

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142. Duncan, Louis D., James 0. Lindberg, and Radon B. Loveland, "AnEmpirical Model of the Vertical Structure of German Fogs,"ASL-TR-0071. November 1980.

143. Duncan, Louis 9 , 1981, "EOSAEL 80, Volume I, Technical Docjmentation,"ASL-TR-0072 January 1981.

144. Shirkey, R. C., and S. G. O'Brien, "EOSAEL 80, Volume II, Jsers Manual,'ASL-TR-0073, January 1981.

145. Bruce, C. W., "Characterization of Aerosol 1onlinea- Effects on aHigh-Power CO2 Laser Beam," ASL-TR-O074, Februery 1981.

146. Duncan, Louis D., and James D. Lindberg, "Air Mass Considerations in Ft.Optical Modeling," ASL-TR-O075, February 1981.

147. Kunkel, Kenneth E., "Evaluation of a Tethered Kite Anemometer,"ASL-TR-0075, February 1981.

148. Kunkel, K. E., et al, "Characterization of Atmospheric Conditions at theHigh Energy Laser System Test Facility (HELSTF) White Sands Missil,Range, New Mexico, August 1977 to October 1978, Part II, OpticalTurbulence, Wind, Water Vapor Pressure, Temperature," ASL-TR-0077,February 1981.

149. Miers, Bruce T., "Weather Scenarios for Central Germany," ASL-':-OO78,February 1981.

150. Coqan, James L., "Sensitivity Analysis of a Mesoscale Moisture Model,".3L-TR-0079, March 1981.

151. Brewer, R. J., C. W. Bruce, and J. L. Mater, "Optoacoustic Spectroscopyof CaH4 at the 9pm and 104m C1202 1 6 Laser Wavelengths," ASL-TR-0080,March 1981.

152. Swingle, Donald M., "Reducible Errors in the Artillery Sound RangingSolution, Pa,'t I: The Curvature Correction" (U), SECRET,ASL-TR-0081, April 1981.

153. Miller, Walter B., "The Existence and Implications of a FundamentalSystem of Linear Equations in Sound Ranging" (U), SECRET,ASL-TR-0082, Arril 1981.

154. Bruce, Dorothy, Charles W. Bruce, and Young Paul Yee, "Expe-imentallyDetermined Relationship Between Extinction and Liquid WaterContent," ASL R-0083, April 1981.

155. Seagraves, Mary Anr, "Visible and Infrared Obscuration Effe.:ts of IceFog," ASL-TR-00)84, May 1981.

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156. Watkins, Wendell R., and Kenneth 0. White, "Wedge Absorption RenoteSensor," ASL-TR-0085, May 1981.

157. Watkins, Wendell R., Kenneth 0. White, and Laura J. Crow, "TurbulenceEffects on Open Air Multipaths," ASL-TR-0086, May 1981.

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