bootstrap beacon creation for overcoming the effects of beacon anisoplanatism in a laser beam...
TRANSCRIPT
Bootstrap beacon creation for overcoming the
effects of beacon anisoplanitism in laser beam
projection system
Aleksandr V. Sergeyev, Piotr Piatrou and Michael C. Roggemann
Department of Electrical and Computer Engineering, Michigan Technological
University,
1400 Townsend Drive, Houghton, Michigan 49931-1295
[email protected], [email protected], [email protected]
1
In this paper we address the problem of using adaptive optics to deliver
power from an airborne laser platform to a ground target through atmospheric
turbulence under conditions of strong scintillation and anisoplanatism. We
explore three options for creating a beacon for use in adaptive optics beam
control: scattering laser energy from the target, using a single uncompensated
Rayleigh beacon, and using a series of compensated Rayleigh beacons. Our
work demonstrates that a using a series of compensated Rayleigh beacons
provides the best beam compensation.
Keywords: artificial laser beacon, turbulence, scintillation, anisoplanitism,
partial compensation. c© 2007 Optical Society of America
2
1. Introduction
Due partly to the success and maturity of astronomical adaptive optical systems,
interest in developing adaptive optical systems for directed energy applications has
developed. The key goal of any adaptive optical system is to compensate for the
wavefront errors induced by atmospheric turbulence. In the present case, we examine
adaptive optical solutions to compensate for turbulence effects in order to deliver a
sufficient level of laser energy from an airborne platform to ground-based receivers.
To overcome the degradation in beam quality caused by atmospheric turbulence, it
is generally necessary to measure and compensate for the phase distortions in the
wavefront. A fundamental problem these systems face is the lack of a suitable beacon
to probe the optical effects of the atmospheric turbulence along the path. In astronomy
a natural star can serve as a beacon, and in other cases a high altitude artificial beacon
can be created. However, in most non-astronomy cases there is no suitable beacon
for wavefront sensing available, and as a result, a beacon must be created artificially.
Due to the desired engagement geometries and turbulence strength along the optical
path of interest, simple strategies for creating a beacon, such as scattering light from
a beacon laser off the target, can result in beacons which are scintillated,5 and more
importantly, significantly larger that the isoplanatic patch in the scene. In this work
we consider a down-looking scenario, in which the aircraft carrying the laser is flying at
various altitudes and pointing the laser beam at a target located at ground level with
a fixed slant path distance of 5000 m.It is important to note that we use conventional
AO methods: Shack-Hartman WFS, LS reconstractor that are intended for use in
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weak turbulence strength conditions to make compensation in strong turbulence. We
present three techniques for beacon creation in a down-looking scenario, and explore
beam control performance tradeoffs:
1. Scattering an initially focused laser beam from the surface of the target.
2. Generating a Rayleigh beacon part way to the target.
3. Applying a novel “bootstrap” technique by placing a series of compensated
Rayleigh beacons between the aperture and the target.
In the first technique the whole volume of the atmosphere between the transmitter
and the target is probed by scattering the beacon laser from the target. In this case,
the beacon is created by the laser beam, propagated through the turbulence, and
scattered from the surface of the target. The second strategy uses a single Rayleigh
beacon which is created at some intermediate distance between the transmitter and
the target. This method allows compensation for part of the atmospheric path, which
in some cases provides improved performance. Lastly, we present a bootstrap beacon
generation technique, in which a series of compensated beacons is created along the
optical path, with the goal of providing a physically smaller beacon at the target
plane. The first beacon is an uncompensated Rayleigh beacon generated relatively
close to the transmitter. We note, that due to the fact that the first beacon is gen-
erated close to the receiver and relatively weakly distorted by the turbulence, it is
statable for wavefront sensing. The back-scattered field from the first beacon carries
information about wavefront errors induced by part of the turbulent atmosphere. This
information is used by the adaptive optical system to precompensate the next beacon
4
to be generated at some greater distance from the aperture. The bootstrapping pro-
cedure continues until the beacon reaches the target. In all cases there is no tracking
information available due to the reciprocity of the optical path,15 and this informa-
tion must be obtained from some other aspect of the scene or target. We conjecture
that a tracker based on a block-matching algorithm using an image of the scene,10,11
may provide sufficiently accurate tracking information. The beacon created using the
first approach is generally larger than the isoplanatic angle for the path, and due to
the scattering from the surface of the target, will also be corrupted by the coherent
laser speckle effect.12 The second approach will generally provide a beam with smaller
angular extent compared to the case of scattering from the surface of the target, even
though only part of the atmosphere along the path was probed by the light returned
from the beacon. Compensation performance of a single Rayleigh beacon as a func-
tion of the position of the beacon is investigated in this work. In order to investigate
compensation performance of a single Rayleigh beacon as a function of the position
of the beacon along the optical path we perform a set of simulations, generating un-
compensated Rayleigh beacons at distance 2.75 km, 3.25 km, 3.75 km, and 4.25 km in
front of the aperture. It was found that the compensation performance depends on the
position of the generated beacon along the optical path. This dependence is especially
pronounced in the case where the Rayleigh beacon is generated at the lower altitudes
probing the strongest turbulent layers of the atmosphere. The bootstrap technique
probes the whole volume of the atmosphere along the path, and provides a suitably
small beacon at a useful distance from the aperture. Compensation performance of
the bootstrap technique was explored as a function of the number of beacons gener-
5
ated along the optical path. We test developed AO system with four different sets of
beacon distributions: 1) [4.25 km, 5 km]; 2) [3.75 km, 4.25 km, 5 km]; 3) [2.75 km,
3.75 km, 4.25 km, 5 km], and 4) [2.75 km, 3.25 km, 3.75 km, 4.25 km, 5 km], where
the numbers in square brackets give the distance of the beacons in kilometers from
the transmitting laser. To represent the turbulent structure of the atmosphere, the
Hufnagel-Valley 57 turbulence model was used.1 To study the performance of the tech-
niques presented here we perform the tests under different turbulence conditions by
placing the platform with the transmitting laser at different altitudes: 1000, 500 and
300 meters, while maintaining a constant distance to the target of 5 km, representing
the cases of mild, moderate and strong turbulence, respectively. The performance is
evaluated by using the average Strehl ratio and the radially averaged intensity of the
beam falling on the target plane. Simulation results show that under most turbulence
conditions of practical interest the bootstrap technique provides better compensation
performance compared to other two techniques.
In order to explore the upper bound of performance for the case of a beacon in the
target plane an ideal point-like beacon placed at the target plane was used. To obtain
the upper bound of performance for single Rayleigh beacon generation technique we
performed a set of simulations for a five kilometer path length, placing the ideal point-
like Rayleigh beacon at the distance 2.75 km, 3.25 km, 3.75 km,and 4.25 km in front
of the aperture.
Power requirements for Rayleigh beacon generation were also investigated in this
work. Calculations presented here are based on computing the number of expected
photodetection events in a circular subaperture of the WFS from Rayleigh backscat-
6
ter given initial power of the source. The functional dependence of the number of
photodetection events per WFS subaperture per integration time as a function of the
laser pulse energy was derived. This functional dependence can be used to find the
optimal laser pulse energy based on the desired photo return. We found that a laser
capable of generating on the order of 3 J of laser pulse energy per pulse is suitable
for the laser projection system described in this work. We also note that calculations
for Rayleigh backscatter lead us to believe that for the lasers with 3 J of laser pulse
energy per pulse and higher the high signal-to-noise(SNR) ratio is obtainable and
therefore wavefront sensor SNR can be ignored.
The remainder of this paper is organized as follows. In the next section we discuss
theoretical considerations for beam projection through the turbulence, specifically
examining a down-looking scenario. The simulation developed to study the perfor-
mance of artificially created beacon using strategies described above is presented in
Section 3. Results are presented in Section 4, power requirements for Rayleigh beacon
generation are shown in Section 5, and conclusions are drawn in Section 6.
2. Theoretical background
Light passing through the turbulent atmosphere becomes distorted. This distortions
are caused by variations in the index of refraction along the optical path of the
beam and wave propagation mechanism. These variations are caused by turbulence-
induced temperature fluctuations in the atmosphere resulting in density changes. In
this section we describe the theoretical characteristics of a laser beam arriving at the
target plane. The impact of turbulence on an optical beam of a given path through the
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atmosphere is commonly characterized by the parameters: ro, θ0, σ2χ ρI , and 〈ρ2
s〉. The
Fried parameter ro is the aperture size beyond which further increases in its diameter
result in no further increase in the resolution of an imaging system.1 The isoplanatic
angle θ0 defines the maximum angle between two optical paths for which the two
paths may be regarded as having approximately the same turbulence distortions.5
The Rytov variance σ2χ is the variance of the log-amplitude fluctuation of the field in
the plane of the receiving optical system, and is a measure of whether the effects of the
turbulence on a particular system is dominated by phase effects. For a a converging
spherical wave centered at the target plane z = 0 the parameters ro, θ0, and σ2χ can
be calculated using the following formulas.5
r0 =
[
0.423 sec(φ)k2
∫ L
0
dzC2
n(z)(z/L)5/3
]−3/5
(1)
θ0 =
[
2.914k2 [sec(φ)]8/3
∫ L
0
dzC2
n(z)z5/3
]−3/5
(2)
σ2
χ = 0.563k7/6 [sec(φ)]11/6
∫ L
0
dzC2
n(z)z5/6(z/L)5/6 (3)
where the wave number is given by k = 2π/λ, λ is the wavelength, h is the altitude
of the propagation path, and φ is the zenith angle. The structure constant C2n(z)
characterizes the strength of the index of refraction fluctuations. The Hufnagel-Valley
profile for the C2n(z), which we used here, is given by.1
C2
n(z) = 5.94 × 10−53(υ/27)2z10e−z/1000 + 2.7 × 10−16e−z/1500 + Ae−z/100 (4)
where A and υ are free parameters.4 The parameter A sets the strength of the tur-
bulence near the ground level and υ represents the high altitude wind speed. Typical
8
values for the A and υ are 1.7 × 10−14m−2/3 and 21 m/s, respectively. Beam spread-
ing and beam wander are the beam counterparts to the image blurring and centroid
jitter. Turbulence scales that are large with respect to the beam size cause tilt, while
turbulence scales that are small relative to the beam size cause beam broadening.
As a result, a long exposure of the beam would result in the superposition of many
realizations of the random wander of the broadened beam, which is an important
consideration for beam pointing and tracking. However, the short-term broadening is
important for pulse propagation and high-energy laser systems which have accurate
trackers. The mean square short-term beam radius of an initially collimated beacon
laser beam focused on the surface of the target 〈ρ2s〉 is given by5
〈ρ2
s〉 =4L2
(kD)2+
4L2
(kρ0)2
[
1 − 0.62(ρ0
D
)1/3]6/5
(5)
where the transverse correlation length of the field ρ0 is related to the Fried parameter
r0 by r0 = 2.1ρ0. The isoplanatic angle projected to the target plane has radius Lθ0/2,
which is referred to as the isoplanatic patch radius ρI
ρI =Lθ0
2(6)
We evaluate beam parameters r0, θ0, σ2χ, ρI , and 〈ρ2
s〉 as as a function of the altitude
z, for wavelength λ = 1.06µm, transmitting lens diameter of D = 0.5 m. The result
of evaluating these parameters for the geometry of interest is shown in Figs 5, 6, 7,
and 8. The structure constant C2n(z) shown in Fig. 4 for low altitudes takes values
close to 10−14 m−2/3, representing fairly strong turbulence conditions. Fig. 5 shows
that r0 varies from 10 cm to 1 m depending on the altitude. Fig. 6 shows that for
our geometry the isoplanatic angle is of the order of 1 µrad if the propagation takes
9
place at low altitudes and reaches 65 µrad at the altitude of 5000 m. Also, from
Fig. 7, it can be seen that the short term RMS beam radius, representing the root
mean square instantaneous spot radius in the target plane after passing through the
atmosphere and focused on the target, at altitudes of the laser platform below 700
m will be bigger than the isoplanatic patch radius. This leads us to conclude that
beacon anisoplanatism will effect on the performance for beacons created by scatte-
ring light from the target.23 In addition, in Fig. 9 we present isoplanatic patch radius
for different altitudes of the laser platform as a function of the slant range. Data
presented in Fig. 9 is used to find the correct position of the beacon in the bootstrap
technique so that the footprint of the last beacon generated at the target plane stays
within the isoplanatic patch and therefore reduce the effect of beacon anisoplanitism.
Fig. 8 demonstrates that significant fluctuations of the field amplitude are expected,
especially at low altitudes. As a result, we conclude that scintillation will be non-
negligible over many paths of practical length for beam projection systems, and that
simulations are an appropriate means of modelling atmospheric optics effects and the
performance of strategies for mitigating turbulence effects. It is evident that there are
certain difficulties and limitations for artificial laser beacon generation for wavefront
sensing and beam control. In the case when the beacon is created by scattering an
initially focused beam from the surface of the target, the footprint of the beacon
laser in the scene is considerably larger than the isoplanatic patch. As a result, light
scattered from a surface in the scene will propagate through many different and only
weakly correlated atmospheric paths on its way back to the aperture. The turbulence
induced abberations from all these paths arrive superimposed at the aperture and
10
hence make computing a useful set of deformable mirror commands based on a wave
front sensor measurements of this field exceedingly difficult. An alternative method
is to generate an uncompensated Rayleigh beacon at some intermediate distance be-
tween the transmitter and the target, by scattering light from atomic, molecular, and
aerosol content in the atmosphere. This method allows compensation for only part
of the atmospheric path, that is, the part between the beacon and the transmitter.
It was shown in6 that generation of a Rayleigh beacon can be effective, and under
some conditions provide results close to those obtained in the case of an ideal point
source beacon in the target plane. For the down-looking geometry examined here the
approach of using a single Rayleigh beacon may be not as effective due to the fact
that the strongest turbulence is located near the ground. A novel bootstrap tech-
nique for artificial beacon creation, which allows dynamic wavefront compensation,
involves formation of a series of compensated beacons at increasing distances from
the aperture. The bootstrap strategy probes the whole volume of the atmosphere us-
ing multiple step precompensation of the beacons, that should help achieve a smaller
footprint of light distribution in the target plane, reduce effects of scintillation, and
beacon anisoplanatism present in other approaches for beacon creation. In the next
section we describe the simulation approach used to compare the performance of the
compensation techniques discussed above.
3. Simulation approach
The main body of the simulation used in all three approaches is a three way propagator
that is summarized by the following steps:
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1. An artificial laser beacon is propagated through the atmosphere from the laser
aperture to the beacon plane.
2. Light is scattered from the surface of the beacon plane, which is modeled as an
incoherent scatterer.
3. Scattered light propagated back through the atmosphere and intercepted by
the aperture is used to form wave front sensor measurements, which are used
to compute deformable mirror commands.
4. A compensated outgoing beam is reflected from the surface of corrected de-
formable mirror model and propagated through the atmosphere back to the
target plane, where performance metrics are computed.
The key parameters of all the simulations whose results will be presented below are
summarized next. The system working wavelength is 1.06 µm; and the transmit-
ter/receiver telescope diameter is 50 cm. The distance to the target was fixed at 5
km, and different propagation angles were specified by changing the aircraft altitude.
Scalar diffraction theory was used to model light propagation. The atmospheric tur-
bulent volume as well as the optical elements were modeled as multiple thin phase
screens for which the mathematical relationship between the incident field Ui(~x, zn)
and the field Ut(~x, zn) after a screen can be described as
Ut(~x, zn) = T (~x, zn)Ui(~x, zn), (7)
where ~x is a two-component coordinate vector in the phase screen plane, zn is the
position of the nth screen along the propagation path, T (~x, zn) = exp(jφ(~x)) is a pure
12
phase transmission function of the screen describing either a random turbulence-
induced phase perturbation or the phase mask associated with an optical element.
Screen-to-screen optical field propagation was performed in Fourier domain:
U(~x, zn+1) = F−1{F [T (~x, zn)U(~x, zn)]H(~f, zn+1 − zn)}, ~x = (x, y), (8)
where
H(~f, zn+1 − zn) = exp
{
j2π(zn+1 − zn)
λ(1 − λ2|~f |2)1/2
}
(9)
is the angular-spectrum propagation transfer function for the distance (zn+1 − zn), ~f
is a spatial frequency domain vector corresponding to ~x, and F and F−1 stand for
direct and inverse Fourier transforms.
To appropriately sample the quadratic phase term in the transmittance functions
Tl(~x) = exp
(
j2π
λ
|~x|2
2f
)
, (10)
associated with either the lens responsible for beam focusing or for the WFS lenslet,
the sampling criterion should satisfy the condition
△xi ≤2λf
3D, (11)
where f and D stand for focal distance and diameter of a lens, respectively. Hence,
we choose for the final sampling period same in all phase screens
△x ≤ min
[lturb1
3, ...,
lturbP
3,
2λf1
3D1
, ...,2λfK
3DK
]
, (12)
where the minimum is taken over all P phase screens and all K lenses present in the
optical system.
13
Given △x, the size of sampling grid N necessary to represent all the frequencies
present in the angular spectrum propagator H(~f,△zn) is found from the criterion
N ≥3λ
(△x)2max
i(zi+1 − zi), (13)
where index i runs over positions of all the atmospheric phase screens and optical
elements. According to the criteria given in Eqs. 12 and 13 a square computational grid
with sampling period △x = 0.0019 mm and size N = 430 was used to appropriately
sample each phase screen and the angular spectrum transfer function given in Eqn. 9.
Unphysical wrap-around error, which arises from light scattered at wide angles
from the rough surface of the target, was strongly attenuated by a set of filter masks
placed on to each turbulence layer, with mask transparency function equal to unity
within the angular extent of the transmitter/receiver aperture and a Gaussian roll-off
outside.
The random phase screens were generated using technique developed by Cochran.9
The parameter r0 is required by the phase screen generator, and needs to be calculated
for each turbulent layer as a function of the altitude. In this simulation the atmo-
spheric path was modelled with 10 equally spaced, different strength phase screens,
with the first phase screen placed in the aperture plane and the last one 500 m away
from the target. The Fried parameter r0 was calculated for each phase screen using
Eqn. 1. We note that integration of the structure constant C2n in the kernel of the
Eqn. 1 is in the direction pointing from the target to the aperture. The laser bea-
con is propagated from the laser aperture through all the phase screens between the
aperture and the beacon plane. The beacon light is then scattered from the surface
14
of the target, for the target plane compensation case, or from the atmosphere in the
case of the Rayleigh beacon and “bootstrap” approaches. Scattering from the target
plane and the atmosphere was modeled by repeatedly multiplying the phase of the
incident field on the surface by a random phase uniformly distributed on (−π, π),
propagating this scattered field back to the aperture, and accumulating the resulting
intensities in the wave front sensor detector plane. This approach models the inco-
herent nature of the scattered field.12 The number of random scattering phases used
here was Nsp = 100. The focal length of the transmitting lens was chosen to match
the propagation path length between the output lens and the required position of the
beacon, so that in the absence of the turbulence, a diffraction-limited spot would ap-
pear if a collimated beam were passed through the lens toward the required location
of the beacon. In the case of delivering the compensated beacon to the target location
the focal length of the lens was set to the total distance between the transmitting
laser and the target. In the bootstrap case, we use a lens with variable focal length
in order to deliver the precompensated beacon to the current required position. The
expression “variable focal length” is used here to describe the adjustment required to
mach the focal length of the lens and the propagation distance to the current position
of the generated beacon. The all three approaches were executed for 100 independent
realizations of the atmosphere, resulting intensity patterns were accumulated and av-
eraged to obtain the final results presented below. In all three techniques we assumed
that the sum of the round trip propagation time and the time required to compute
deformable mirror commands was shorter than the time required for the turbulence
to change significantly. That assumption allowed us to use the same phase screens for
15
the outgoing beacon illumination laser, the returning scattered light, and the outgo-
ing compensated laser beam. Next we describe simulation models of the tilt removal
system,the Shack-Hartman wavefront sensor, the deformable mirror model, and the
least-square wavefront reconstructor used in this work.
3.A. Maximum Tracker-Tilt Correction Model
Wavefront tilt shifts the center of the focused image by an amount directly propor-
tional to the amount of wavefront tilt. Usually tilt correction is achieved separately
from the correction procedure for higher order of the turbulence-induced abberations.
In our simulation we exclude the tilt from our consideration assuming that an inde-
pendent beam steering system that stabilizes the spot position already operates on
the laser platform, and focuss on tilt-removed or “short-exposure” performance of the
laser beam control system. We do not make any specific assumptions about principle
of operation of this independent tilt control system or its key characteristics such
as residual error. On the other hand, the work of such a system should be imitated
during the simulation of the compensation techniques described in this work. We do
this imitation by using an iterative “target-in-the-loop” algorithm that measures the
position of the target intensity distribution maximum and adds tilt correction to the
DM such that to enforce the maximum to be at the origin. Two features of this al-
gorithm should be emphasized: 1) it is not realistic because the information about
target intensity distribution maximum position is generally not available, so the al-
gorithm can be used only as imitation of a real tilt control system; 2) the residual tilt
error of this algorithm corresponds to just a fraction of a pixel in the target plane,
16
i.e. it is much smaller than the residual error of any real tilt control system, so the
“short-exposure” performance results of our simulations represent the upper limit for
the overall beam control system performance.
3.B. Shack-Hartman Wavefront Sensor
The wavefront sensor measures the lateral displacement of the centroid of the inten-
sity spot in the focal plane. When an incoming wavefront is planar, all images are
centered on the optical axis of the lenslets. When aberrations are present, the im-
ages are displaced from their nominal positions. Displacements of image centroid in
two orthogonal directions are proportional to the average wavefront slopes over the
subapertures.
Shack-Hartmann wave front sensor is represented by its lenslet transmission func-
tion
Twfs =1
d2
S∑
i=1
rect(~x− ~xi
d) exp{−j
k
2fl
|~x− ~xi|2}, (14)
where S is the number of subapertures of the wavefront sensor, rect(~x) is a 2-D
rectangular function, fl is the focal length of a lenslet, ~xi is the center of the ith
subaperture and d is the length of the subaperture. The WFS readout ~s proportional
the local wave front tilts was modeled as an output of a four-pixel CCD cells centered
around each subaperture using the standard quad rule:
sx =(I1 + I2 − I3 − I4)
(I1 + I2 + I3 + I4), (15)
sy =(I2 + I3 − I1 − I4)
(I1 + I2 + I3 + I4),
where sx, sy are x- and y-components of the readout from a single subaperture, {Ii}4i=1
17
are the intensities in each of four pixels in the quad cell. The local wave front tilts can
be found from the readout given by Eq. 15 after calibration process associated with
the DM-to-WFS interaction matrix computation as is described in the next section.
A wave-optics model of the Hartman sensor was used7 with subaperture sides in
the pupil of length 3.8 cm, yielding a total of 137 subapertures in the pupil. The
physical side length of the lenslets modeled was 180 µm, and the focal length of the
lenslets was 7 mm.
3.C. Deformable Mirror Model
A single DM used for phase correction is optically conjugated to the exit pupil of the
projector telescope. The linear model of the DM mirror surface is given by:1
φ̂dm(~x) =M∑
i
~̂uri(~x) (16)
where ~̂u is the control signal applied to the ith actuator of the DM and {ri(~x)}Mi=1
are the DM influence functions. A continuous face sheet DM was assumed for our
simulation, with influence functions approximated by bilinear splines:
ri(~x) = tri[x− xi
d
]tri[y − yi
d
](17)
where
tri(x) =
1 − |x| if |x| ≤ 1
0 otherwise
placed over a square grid −→x iNi=1 with grid size equal to the inter-actuator spacing.
The deformable mirror was modeled using a Cartesian array of actuators with bilinear
spline influence functions separated by 3.8 cm, yielding a total of 164 active actuators
18
inside the pupil. The base width of the influence functions was twice of their separation
distance which leads to 7.6 cm. Fried geometry of the WFS and DM mutual layout
is shown in Fig. 10.
3.D. Least-Squares Wavefront Reconstructor
In this work we used the least-squares wavefront reconstructor to map the measured
wavefront slopes ~s given by Egn. 15 into DM commands. This is motivated by the
desire to use a reconstruction algorithm that does not rely on knowledge of turbulence
statistics often unavailable in air-to-ground applications. A least-squares estimator
computes the optimal set of DM control commands ~u as
~̂u = arg min~u
||~s−G~u||2, (18)
where G is the DM-to-WFS influence matrix that gives the WFS readout in response
to a command applied to the DM. The G-matrix can be found by the WFS/DM cali-
bration process when a unit amplitude commands are sent sequentially to a single DM
actuator and the corresponding WFS readouts, that are equal to the corresponding
columns of the G-matrix, are recorded. This process was modeled using the angular
spectrum propagation technique by applying the phase screen
Ti(~x) = Twfs(~x)ri(~x), i = 1, ...,M (19)
to a plane wave, propagating the result to the WFS focal plane and forming WFS
readouts by Eq. 15. Here, Twfs, ri are the WFS transmittance and ith DM influence
functions given by Eqs. 14 and 17, respectively.
19
4. Results
In this section we evaluate compensation performance of developed AO system using
proposed in this work beacon generation techniques: 1) bootstrap technique; 2) target
plane compensation technique; and 3) single Rayleigh beacon generation technique.
First, we present the result of beacon creation using target plane compensation tech-
nique and compare it with the uncompensated beacon generated at the target plane.
Laser platform altitude for this case was placed at 300 m representing strong turbu-
lence strength conditions. Fig. 11 show short-exposure target plane intensities of the
uncompensated and target plane compensated beacons. The circles drown on both
figures represent an isoplanatic patch. From Fig. 11(a) we observe that the generated
beacon is strongly corrupted by atmospheric turbulence. Also, due to the tilt the
centroid of beacon is shifted from the origin. Inspection of Fig. 11(b) shows that the
generated beacon using target plane compensation technique is significantly bigger
than the isoplanatic patch which is consistent with theoretical calculations presented
in Fig 7 and, as a result, the effect of the beacon anisoplanitism will affect the com-
pensation performance. In order to reduce anisoplanatic nature of the generated at
the target plane beacon the dynamic beacon creation technique was implemented. In
Fig. 12 we demonstrate the beacon formation process along the optical path using
bootstrap compensation technique. Laser platform was placed at 300 m to simu-
late strong turbulence strength conditions. Fig 12(a-e) show five beacons created at
[2.75km, 3.25km, 3.75km, 4.25km, 5km] from the aperture. Circles drown on the top
represent isoplanatic patch radii for the current position of the beacon. Fig 12(f)
20
shows the final beacon generated at the target plane. Only the first uncompensated
beacon shown in Fig 12(a) is not within the isoplanatic patch but the rest 4 beacons
and, what is the most important, the final beacon generated at the target plane are
indeed within the isoplanatic patch that should significatively reduce the effect of
beacon anisoplanitism. As we mentioned earlier in this paper, it was of our interest to
study the compensation performance of a single Rayleigh beacon as a function of the
position of the generated beacon along the optical path and compare its compensa-
tion performance with the results obtained from the target plane and the bootstrap
compensation techniques. To fully investigate the performance of a single Rayleigh
beacon technique we tested the AO system under different turbulence strength con-
ditions. We performed a set of simulations, generating an uncompensated Rayleigh
beacon at different locations along the optical path. Next, we summarize and analyze
the compensation performance of the beacon generation techniques presented in this
work. In Table 1 we present Strehl ratios for various beam compensation scenarios
as a function of the laser platform altitude. To represent “mild”, “moderate”, and
“strong” turbulence strength conditions we placed the laser platform at the altitude
1000, 500, and 300 meters respectively, and a constant 5000 slant range between the
transmitter an the target for all cases. In order to explore the upper bound on perfor-
mance of the simulated AO system under different turbulence strength conditions, we
performed a set of simulations for a five kilometer path length, placing an ideal point-
like beacon at the target location. A Rayleigh beacons were generated at the distances
of 2750 m, 3250 m, 3750 m, and 4250 m from the laser platform. In the bootstrap
technique 4 sets of beacons were used with the following distributions along the op-
21
tical path: [4.25km, 5km], [3.25km, 4.25km, 5km], [3.25km, 3.75km, 4.25km, 5km], and
[2.75km, 3.25km, 3.75km, 4.25km, 5km]. In the target plane compensation technique
the beacon was generated directly at the target location probing whole volume of the
turbulent atmosphere in one step. Based on the data presented in Table 1 we make
a few conclusions. It was found that under different turbulence strength conditions
the compensation performance of a single Rayleigh beacon depends on the distance
of the generated beacon from the aperture. A single Rayleigh beacon generated at
the farthest distance from the transmitting aperture probes the strongest turbulent
layers and, as a result, provides better compensation performance. For example, for
the Rayleigh beacon generated at the distance 2750 m from the transmitter under
mild, moderate, and strong turbulence strength conditions, Strehl ratios are 0.66,
0.34, and 0.14, respectively. On the other hand, for the Rayleigh beacon generated at
the distance 4250 m from the transmitter under mild, moderate, and strong turbu-
lence strength conditions, Strehl ratios are 0.77, 0.5, and 0.29. Comparing all three
techniques we observe that the bootstrap technique in all cases provides the best
compensation performance. The advantage of the bootstrap technique is especially
pronounced under strong turbulence strength condition providing about 30 percent
of improvement over the target plane compensation technique and about 32 present
over the best case of a single Rayleigh compensation technique. This improvement,
as expected, is not that significant under mild turbulence strength conditions which
is consistent with the theoretical calculations presented in Fig 7 showing that at 1000
m altitude of the laser platform the beacon generated directly on the target plane is
within the isoplanatic patch and therefore the effect of the beacon anisoplanitism is
22
negligible. Confidence in the results was obtained computing the standard divination
of the strehl ratios for each case and was always within 0.01 − 0.013 range.
5. Power Requirements for Rayleigh Beacon Generation
For practical applications, it is important to estimate the power required to generate
a single Rayleigh beacon at some distance from the transmitting laser source which
will allow wavefront sensor measurements to be made with satisfactory signal-to-
noise ratio. In this section I present the outline of calculations conducted in order to
estimate the power requirements for a single Rayleigh beacon as a function of the laser
altitude and the slant range between the transmitting laser and generated beacon. To
fully understand the result presented in this section some physical understanding of
the nature of scattering is required.
5.A. Types of Scattering
Scattering at the atomic level occurs when a photon of incident radiation is annihilated
while a photon of scattered radiation is created. There are two types of scattering
that may occur: elastic and inelastic. If the frequency of the scattered radiation is
the same as the incident radiation the scattering is defined as elastic. If the quantum
state of an atom is changed in the process, then the emitted radiation is changed in
frequency, and the scattering is said to be inelastic. Scattering from larger particles
in the atmosphere is elastic. Different modes of scattering can be summarized in four
main groups:
1. Rayleigh scattering, in which radiation scattered from the atoms or molecules
23
does not experience the change in a frequency.
2. Raman scattering, in which scattered radiation has change in frequency due
to the change in the vibrational or rotational quantum states of the atoms or
molecules.
3. Mie scattering, in which radiation is scattered from small particles or aerosols
of size comparable to the wavelength of the incident radiation, with no change
in frequency.
4. Resonance scattering, in which radiation matched in frequency to a specific
atomic transition is scattered, with no change in frequency.
5.B. A Lower Bound on Power Requirements
Raman scattering is very weak. Typically, only one photon out of 107 is Raman
scattered. Resonance scattering requires tuning the laser on the frequency closely
comparable to the internal rotational or vibrational frequency present in a specific
atom or molecule. The presence of dust, fog, haze, and clouds causes the Mie
scattering, which occurs mostly in the lower atmosphere(below 35 kilometers), and
varies unpredictably. It should be noted that the Mie scattering cross-section can
have a large value, producing a strong backscatter. In practice, it is important to
produce a stable, reliable beacon. The generation technique for a Rayleigh beacon
should not rely on surrounding atomic and molecular content, and unpredictable
events such as presence of clouds, haze, dust or fog. Therefore, it is reasonable to
count on the always present, elastic Rayleigh scattering. As a result, I based the
24
calculations for power requirements for a Rayleigh beacon generation only on elastic
Rayleigh scattering excluding impact of other types of scattering. The result of
our calculation forms a lower bound on the required power for Rayleigh beacon
generation, and occasionally the presence of other types of scattering may improve
the final result by boosting the scattered energy.
5.C. Power Requirements Calculation
The process of using a light beam to probe a medium using backscattered energy as
a function of range is known as LIDAR (light detection and ranging). The LIDAR
equation13 defines the energy detected at the receiver because of the scattering process
as a light propagates through the media. To calculate the power backscattered into
receiver we start by defining the angular scattering cross-section per molecule for
Rayleigh scattering σ(θ) as:
σ(θ) = σ0
1 + cos2(θ)
2(20)
where
σ0 =4π2(n0 − 1)2
N20λ
4(21)
λ is the wavelength, n is the refractive index of the air, N is the number density of
molecules and the subscript 0 denotes sea-level values. For backscattering θ = π. The
scattering coefficient for losses from a beam as a function of an altitude h is given by3
β(h) = β0
ρ(h)
ρ0
(22)
25
where ρ is the mass density of the air, h is altitude and scattering coefficient for losses
from a beam at sea level
β0 =8π
3N0σ0 (23)
The effect of air density variations for altitudes ranging from 0 and 5 kilometers are
studied here.
The transmission efficiency η of a beam projected at the zenith angle ψ to the range
z is calculated using
η(z, ψ) = exp[−β0ρ0
∫ z
0
dhρ(h)]
(24)
The power P (z, t) at the range z is
P (z, t) = P0(t− z/c)η(z, ψ) (25)
where P0 is the power transmitted by the laser. The power Pr backscattered into the
receiver is
Pr(t) =∫
∞
0
dzP0(t− 2z/c)η2(z, ψ)βr(z, ψ) (26)
where
βr(z, ψ) = σ0N0
Ar
z2
ρ(z cosψ)
ρ0
(27)
where Ar is the area of the receiving aperture.
Finally, the energy received from scattering with the range gate △z is3
E =∫
2Z/c+△z/2
2Z/c−△z/2
dtPr(t) =∫
∞
0
dz∫
2Z/c+△z/2
2Z/c−△z/2
dtP0(t− 2z/c)η2(z, ψ)βr(z, ψ) (28)
where Z is the mean range associated with the range gate. The physical meaning of
the laser beacon range gate is visualized in figure 17.
26
The angular size of a beacon formed at the focus of a converging beam is
determined by the depth of the beam covered by the range gate in the receiver.
5.D. Power Optimization for Rayleigh Beacon Generation
To minimize the energy requirements the range gate of the receiver should be chosen
to use the greatest possible scattering depth. It was shown13 that the maximum
scattering depth is calculated using
△z =2△αz2Dp[
D2p − (z△α)2
] (29)
where △α is the angular size of the beacon and Dp is the diameter of the laser projec-
tion aperture. The optimum angular size of the beacon is determined by the subaper-
ture size of the wavefront sensor, or by the value of Fried parameter r0, whichever is
smaller. The angular size of a beacon as a function of r0 can be expressed as:
△α = 2.44λ
r0(30)
when △α is limited by the turbulence, the maximum value of △z may be approxi-
mated as
△z ≈4.88λz2
Dpr0(31)
To maximize the probability that incident photon will be scattered and captured by
the receiver the receiver gate range should be adjusted appropriately. The optimal
receiver gate ranges were calculated as a function of the beacon position along the
optical path using Eqn 31 and are presented in the Table 2.
27
5.E. Simulation Details and Results
The theoretical considerations discussed above are conveniently embedded in the
widely available MATLAB tool box AOTOOLS 3 that was used to evaluate power
requirements for Rayleigh beacon generation. As it was mentioned earlier in this
section the laser energy delivered to the beacon location causes inelastic Rayleigh
scattering from atoms and molecules. Backscattered photons are detected as photo
events by the CCD. The number of photo-detection events (PDE) is directly related
to the laser pulse energy. We investigate the dependence of the backscattered photo
events detected by the CCD on the laser pulse energy of the transmitting laser. It
should be noted that the total energy per pulse is the integration of the power over the
duration of range gate. Reference information for the typical lasers used for Rayleigh
beacon generation in lidar systems and their values can be found in.13 In our simula-
tion the following parameters of the AO system were used. The laser operated at the
wavelength of 1.06 µm. In this simulation the laser pulse energy range was restricted
between 0.1 and 15 joules with the pulse duration equal to 1µsec, that corresponds
to 300 meters in length, but calculations can be easily extended for the lasers with
different power. Optical efficiency of the system output, defined as the fraction of laser
photons that exit the transmitter, was idealized and set to unity. Optical efficiency of
the system input, defined as the fraction of backscattered photons entering the aper-
ture that reach CCD, was considered lossless and set to unity. Quantum efficiency,
that is the fraction of photons striking the CCD that result in a photo detection
event was set to 0.8. The receiving aperture diameter was 0.5 meters. The receiver
28
gate range was adjusted for different slant ranges to its optimal value according to
the Table 2.
As it was mentioned earlier in this section, our goal was to estimate the power re-
quirements for a single Rayleigh beacon generation as a function of the laser altitude
and the slant range between a transmitting laser and generated beacon. It was shown
in Eqn. 24, that the transmission efficiency of the atmosphere is a function of a zenith
angle and the initial altitude of the laser platform. Therefore for the different initial
positions of the laser platform, the outgoing laser radiation will experience different
transmission of the atmosphere. To investigate this effect for the wide spectrrange
of zenith angles we consider three cases by placing the laser platform at 3000, 1500
and 500 meters above the sea level. Figures 13, 14, and 15 demonstrate functional
dependence of number of photo detection events per WFS subaperture per laser pulse
for different altitudes of the laser platform on the transmitting laser pulse energy. It
was also of interest, to investigate the number of photo detection events at the re-
ceiver for the same laser pulse energy but different positions of the beacon along the
optical path. To investigate effect of the slant range Rayleigh beacons were generated
at 4500, 3000, 1500, and 500 meters from the aperture. Optimal integration time
for each slant range was chosen in accordance to Table 2. The number of PDE as a
function of the laser pulse energy for different positions of the beacon is emphasized
in Figures 13, 14, and 15 with different line styles. It is interesting to note that for
beacons generated at 500 and 3000 meters it takes the same laser pulse energy to
observe a similar number of PDE. In my opinion, a reasonable explanation for this
effect would be a trade off between number density of the molecules at lower altitude
29
and the optimal receiver gate range, but more work is required to fully understand
this. The accuracy of wavefront sensing depends on the subaperture slope measure-
ments which are corrupted by shot noise. Shot noise is characterized by a standard
deviation given by1
σn =0.74πη
(K̄w)1/2d, (32)
where η is a parameter accounting for imperfections of the detector array used in
focal plane of the WFS, K̄w is the average number of photon events per WFS slope
measurement, and d is the subaperture side length. The factor η is greater than or
equal to unity, and η is unity only in the ideal case of a perfect detector array. For
the computational results of this work I assume η = 1.2. We calculated the standard
deviation of shot noise based on the photo-detection events. The calculations were
performed for a Rayleigh beacon generated at the distance 4500 meters from the
transmitter as a function of the laser pulse energy. As it was mentioned earlier, the
outgoing laser radiation experiences different transmission through the atmosphere
for the different altitudes of the laser platform. To investigate this effect we consider
three cases by placing laser platform at 3000, 1500 and 500 meters above the sea level.
The result of the calculations are shown in Fig 16
Inspection of Fig. 16 shows that if a laser with pulse energy less then 1 J is used
to generate an artificial laser beacon, slope measurements will be corrupted by a shot
noise with a standard deviation greater than 0.15. Another words, the laser with pulse
energy less then 1 J is not capable of providing signal-to-noise (SNR) ratio for which
shot noise can be ignored. On the other hand, the beacon generated by the laser with
30
pulse energy greater then 3 J can generate SNR at which level it can be safe to ignore
the effect of shot noise.
The results presented in this work provide the future user with a convenient and
efficient tool in identifying the tradeoffs in the laser power the efficiency of the receiver
or otherwise. This tool is helpful in finding the optimal laser pulse energy based on
the required photon return.
6. Conclusions
Three techniques for artificial laser beacon creation in look down, shoot down scenario
for various turbulence conditions were explored in this work. Performance of three
techniques: scattering from the surface of the target, generating Rayleigh beacon at
some distance from the target, and dynamic bootstrap beacon creation technique for
wave front sensing and deformable mirror control were compared with each other and
also with an ideal case of a point source beacon located at the target plane. Under
different turbulence conditions it was found that novel bootstrap technique provides
higher Strehl ratio compare to the other compensation techniques examined in this
work. We have only examined least squares phase reconstruction approach, but it
is likely that wave control improvements would result from use of more advanced,
branch point reconstructor. We conjecture that it might be possible to use presented
bootstrap technique in conjunction with the approach based on the contrast opti-
mization. Presented here novel bootstrap technique involves generation of multiple
Rayleigh beacons along the propagation path and the power requirements for mak-
ing a single Rayleigh beacon is required to understand the performance tradeoffs and
31
therefore have been investigated as a function of the laser altitude and the slant range
between a transmitting laser and generated beacon. Results for power requirements
for Rayleigh beacon generation presented here are based on computing the number
of expected photodetection events in a circular aperture from Rayleigh backscatter
giving initial power of the source. We found that a laser capable of generating on the
order of 3 joules of laser pulse energy per pulse is suitable for the laser projection
system described in this work. There are practical challenges arising with implemen-
tation of the presented in this work approaches for a beacon generation. First of all,
creating a beacon using atmospheric backscatter is energy inefficient operation, and
as a result required beacon laser powers may be exceedingly high. Secondly, the usage
of high power pulse lasers create additional complications related to the hardware re-
quirements. Also propagation of high-energy laser beams through the atmosphere at
a laser wavelength of λ = 1.06 µm is limited by thermal blooming due to aerosol ab-
sorption. Finally, in both strategies for creating the artificial beacon: scattering light
from a surface of the target or in the scene, and use of atmospheric backscatter such
as in case of a Rayleigh beacon, there is no tracking information available from the
beacons, and hance tracking information must be obtained from some other aspect
of the scene or target.
32
Acknowledgements
This research was supported by the Air Force Office of Scientific Research under a
Multiple University Research Initiative lead by the University of California at Los
Angeles, contract number F49620 − 02 − 01 − 0319.
33
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36
Command
processor
for DM
AO system located
on the transmitter
side.
Slant range
5000m
Altitude
3000m
Beam
splitter
Target
DM
WFS
Compensated Beacon
at the Target Plane
Target Plane
Fig. 1. Creating an artificial beacon by scattering the laser beam from the
surface of the target.
37
Command
processor
for DM
AO system located
on the transmitter
side.
Slant range
5000m
Altitude
3000m
Beam
splitter
Target
Uncompensated
Rayleigh
Beacon
DM
WFS
Compensated Beacon
at the Target Plane
Target Plane
Fig. 2. Generating a Rayleigh beacon part way to the target.
38
Command
processor
for DM
AO system located
on the transmitter
side.
Altitude
3000m
Beam
splitter
Target
Uncompensated Rayleigh
Beacon
First Dynamically Precompensated
Beacon
Second Dynamically Precompensated
Beacon
Dynamically Compensated
Beacon at the Target
DM
WFS
Target Plane
Fig. 3. Novel “Bootstrap” beacon generation technique.
39
0 1000 2000 3000 4000 5000
10−16
10−15
10−14
10−13
Altitude, h(meters)
Cn2 (h
),m
−2/
3
Cn2 for HV57
Fig. 4. Structure constant C2n as a function of altitude.
40
0 1000 2000 3000 4000 50000.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
1.1
Altitude,h(meters)
r 0,met
ers
r0(h)
Fig. 5. Fried parameter r0 as a function of altitude.
41
0 1000 2000 3000 4000 50000
1
2
3
4
5
6
7x 10
−5
Altitude,h(meters)
θ 0(rad
)
θ0(h)
Fig. 6. Isoplanatic angle θ0 as a function of altitude.
42
0 1000 2000 3000 4000 50000
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
0.18
Altitude, h(meters)
[<ρ s2 >
]1/2 a
nd ρ
I, met
ers
[<ρs2>]1/2 and ρ
I as a function of h
[<ρs2>]1/2
ρI
Fig. 7. Isoplanatic patch radius ρI and Mean square instantaneous spot radius
in the target plane 〈ρ2s〉 as a function of altitude.
43
0 1000 2000 3000 4000 50000
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
Altitude,h(meters)
σ2 χ
σ2χ(h)
Fig. 8. Rytov variance σ2χ as a function of altitude.
44
0 500 1000 1500 2000 2500 3000 3500 4000 4500 50000
0.01
0.02
0.03
0.04
0.05
0.06
0.07
0.08
Slant distance from receiver L, m
Isop
lana
tic p
atch
rad
ius
ρ I, m
ρI(L)
Altitude 200 m
Altitude 300 m
Altitude 500 m
Altitude 1000 m
Altitude 2000 m
Fig. 9. Isoplanatic patch radius ρI in the target plane for different altitudes of
the laser platform as a function of the slant range.
45
−1 −0.5 0 0.5 1
x 10−3
−1
−0.5
0
0.5
1
x 10−3
x, m
y, m
Fig. 10. Fried geometry of the WFS and DM mutual layout. Crosses in the
vertices of the square grid represent DM actuators location and crosses in the
centers represent WFS subapertures locations.
46
x, m
y, m
Uncompensated
−0.05 0 0.05 −0.025 0.025
−0.05
−0.025
0
0.025
0.05
(a)
x, m
y. m
Compensated
−0.05 0 0.05 −0.025 0.025
−0.05
−0.025
0
0.025
0.05
(b)
Fig. 11. a)Uncompensated beacon created at the target plane. b)Beacon cre-ated using target plane compensation technique. Laser platform altitude was300 m
47
x, m
y, m
Beacon generated at 2.75 km
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
x, m
y. m
Beacon generated at 3.25 km
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
(a) (b)
x, m
y, m
Beacon generated at 3.75 km
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
x, m
y, m
Beacon generated at 4.25 km
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
(c) (d)
x, m
y, m
Beacon generated at 5 km
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
x, m
y, m
Final beacon generated at the target
−0.02 −0.01 0 0.01 0.02
−0.02
−0.01
0
0.01
0.02
(e) (f)
Fig. 12. Beacons formation process along the optical path using bootstrapcompensation technique under strong turbulence strength conditions. Laserplatform altitude was 300 m. Figures a) − e) show five beacons created at[2.75km, 3.25km, 3.75km, 4.25km, 5.0km] from the aperture. Circles drown onthe top represent isoplanatic patch radii for the current location of the beacon.f shows the final beacon generated at the target plane.
48
0 5 10 150
0.5
1
1.5
2
2.5
3
3.5
4x 10
6
Laser pulse energy(Joules)
Num
ber
of p
hoto
dect
ion
even
ts(P
DE
) pe
r W
FS
sub
aper
ture
# PDE(Laser Pulse Energy), Laser Altitude 3000 m
Beacon at 4500 mBeacon at 3000 mBeacon at 1500 mBeacon at 500 m
Fig. 13. Number of photo-detection events per WFS subaperture per laserpulse for different altitudes of the laser platform as a function of the laserpulse energy. Altitude of the laser platform is 3000 meters.
0 5 10 150
0.5
1
1.5
2
2.5
3
3.5
4x 10
6
Laser pulse energy(Joules)
Num
ber
of p
hoto
dect
ion
even
ts(P
DE
) pe
r W
FS
sub
aper
ture
# PDE(Laser Pulse Energy), Laser Altitude 1500 m
Beacon at 4500 mBeacon at 3000 mBeacon at 1500 mBeacon at 500 m
Fig. 14. Number of photo-detection events per WFS subaperture per laserpulse for different altitudes of the laser platform as a function of the laserpulse energy. Altitude of the laser platform is 1500 meters.
49
0 5 10 150
0.5
1
1.5
2
2.5
3
3.5
4x 10
6
Laser pulse energy(Joules)
Num
ber
of p
hoto
dect
ion
even
ts(P
DE
) pe
r W
FS
sub
aper
ture
# PDE(Laser Pulse Energy), Laser Altitude 500 m
Beacon at 4500 mBeacon at 3000 mBeacon at 1500 mBeacon at 500 m
Fig. 15. Number of photo-detection events per WFS subaperture per laserpulse for different altitudes of the laser platform as a function of the laserpulse energy. Altitude of the laser platform is 500 meters.
50
0 5 10 150
0.1
0.2
0.3
0.4
0.5
0.6
0.7
Laser pulse energy(Joules)
σ nσ
n as a Function of the Laser Pulse Energy , Slant Range is 4500 m
Laser altitude 3000 mLaser altitude 1500 mLaser altitude 500 m
Fig. 16. The standard deviation of shot noise for Rayleigh beacon generated atthe distance 4500 meters from the transmitter as a function of the laser pulseenergy. − denotes the case of the laser platform located at the altitude 3000meters; .− denotes the case of the laser platform located at the altitude 1500meters, and −− denotes the case of the laser platform located at the altitude500 meters
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Converging
laser beam
Laser beacon
range gateTransmitting
aperture
Focal distance
Fig. 17. Geometry of Rayleigh beacon.
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0 500 1000 1500 2000 2500 3000 3500 4000 4500 50000.7
0.8
0.9
1
1.1
1.2
1.3
1.4
Altitude h, meters
Atmospheric density versus altitude
Den
sity
of t
he a
ir ρ,
kg/
m3
Fig. 18. Density of the air as a function of the altitude.
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Compensation Technique Altitude300 500 1000
Point-like beacon 0.44 0.74 0.89at the target planeBootstrap[4.25 5.0] 0.36 0.63 0.86[3.25 4.25 5.0] 0.36 0.64 0.86[3.25 3.75 4.25 5.0] 0.38 0.65 0.87[2.75 3.25 3.75 4.25 5.0] 0.39 0.65 0.87Target Plane 0.31 0.60 0.84Rayleigh[2.75] 0.14 0.34 0.66[3.25] 0.18 0.40 0.68[3.75] 0.22 0.44 0.73[4.25] 0.29 0.5 0.77Uncompensated 0.05 0.21 0.54
Table 1. Strehl ratios for various beam compensation scenarios as a func-tion of the laser platform altitude. A Rayleigh beacon were generated at thedistances of 2750 m, 3250 m, 3750 m, and 4250 m from the laser platform.In the bootstrap technique 4 sets of beacons were used with the followingdistributions along the optical path: [4.25km, 5km], [3.25km, 4.25km, 5km],[3.25km, 3.75km, 4.25km, 5km], and [2.75km, 3.25km, 3.75km, 4.25km, 5km].Standard deviation of the strehl ratios calculated for each computation waswithin 0.01 − 0.013 range.
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