Abstract
A laser beam propagating to a remote target through atmospheric turbulence acquires intensity fluctuations. If the target is cooperative and provides a coherent return beam, the phase measured near the beam transmitter and adaptive optics, in principle, can correct these fluctuations. Generally, however, the target is uncooperative. In this case, we show that an incoherent return from the target can be used instead. Using the principle of reciprocity, we derive a novel relation between the field at the target and the returned field at a detector. We simulate an adaptive optics system that utilizes this relation to focus a beam through atmospheric turbulence onto a rough surface.
© 2016 Optical Society of America
A laser beam propagating through atmospheric turbulence acquires phase aberrations from turbulent fluctuations in the refractive index. These aberrations can quickly develop into intensity fluctuations, degrading the beam profile incident on a remote target [1–5]. In principle, adaptive optics can correct for the phase aberrations if the turbulent channel is reciprocal, a property of optical configurations in which the point spread function is invariant with respect to the interchange of the source and receiver [5–7]. One adaptive optics configuration utilizes a cooperative target that provides a spatially coherent emitter on or near the target. This is essentially a beacon or guide star [5,8]. A wavefront sensor, placed near the beam transmitter, measures the phase of light received from this emitter. If the conjugate field is transmitted, it reproduces the emitter’s irradiance profile at the target. In the special case that the target emitter is point-like, the measured field provides the turbulent channel’s point spread function, and the target can be illuminated with a desired irradiance profile in the vicinity of the emitter.
Often there is no coherent emitter at or near the target, the state of the turbulent channel remains unknown, and one must rely on a reflection or scattering from the target. For normal-incidence mirror-like reflections, the light received at the wavefront sensor has passed through the turbulent channel twice, and the phase aberration acquired in each pass cannot be explicitly determined. Scattering from a rough surface adds a further complication. These surfaces scramble the beam phase such that the reflected beam loses its spatial coherence. In spite of these complications, we show here that an adaptive optics system can use the incoherent return to correct phase aberrations and focus the beam onto the target. In particular, we use the principle of reciprocity to derive a novel relation between the field incident upon a reflector and the field detected by a point receiver. The derivation considers a double pass through the turbulent channel: propagation from the source to the target and back to the detector, making it especially suitable for uncooperative targets. Simulations of an adaptive optics system using the relation demonstrate enhancements in both the on-target intensity and power in the bucket.
We begin by using reciprocity to derive a relation between the field incident upon a reflector and the field detected by a point receiver. While the relation is general to any reciprocal optical configuration, we discuss it here in the context of focusing a laser beam through atmospheric turbulence onto a target that provides a spatially incoherent return. Figure 1 displays the reciprocity preserving geometry considered throughout. The beam starts at the transmitter plane, propagates through the turbulent channel, and undergoes scattering at the target plane. The scattered beam is collected in the receiver plane, where it is focused to the detector. The transmitter and receiver planes coincide, creating a monostatic channel. Both an aperture and phase modulator are located in the transmitter/receiver plane. A thin lens with focal length is centered at distance from the detector and transmitter/receiver planes.
We express the transverse electric field, , as a carrier wave modulating a slowly varying envelope, , where . Since we are only interested in the electric field envelope at specific planes, we adopt the shorthand , , , and for the complex electric field envelopes at the detector, transmitter, receiver, and target, respectively, where , , and are the associated transverse coordinates. The spatial coordinates and fields are normalized by and , respectively, where is the peak intensity of the outgoing beam. The function describes the transfer function of the aperture and phase modulator in the transmitter/receiver plane, which can be any complex, square integrable function.
The initial envelope of the transmitted beam can be expressed as the field of a point source located at propagated from the detector plane to the transmitter plane and filtered by the function :
We denote the point spread function, or Green’s function, for propagation from the transmitter to the target as . In terms of the Green’s function, the electric field envelope at the target is then given by
which, upon making use of Eq. (1), provides In general, the target modifies both the amplitude and phase of the incident field, such that the reflected field has the initial profile , where is a real square integrable function, and is real. Denoting as the Green’s function for propagation from the target to the receiver, we have We stress that can represent any phase shift imparted upon reflection.Back at the receiver plane, the field passes through the aperture and phase modulator and propagates from the front focal plane of the lens to the back focal plane, coinciding with the detector plane. The resulting envelope at the detector is then
Using Eq. (4), we can rewrite this as If the channel between the transceiver and target is reciprocal, the Green’s function for propagation from the transmitter plane to the target plane is equal to the Green’s function for propagation from the target plane to the receiver plane [9]: . If we observe the field at the location , we can write Eq. (6) in terms of the envelope at the target plane described by Eq. (3), which gives the final result, Recall that the location is the location of the point source corresponding to the transmitted beam and can be determined by the tilt of the transmitted beam. Experimentally, this location can be found through the enhanced backscatter phenomenon [10].Equation (7) relates a single quantity measured by the detector, , to the field at the target plane , with information about the optical configuration contained only implicitly in . The remaining factor, , captures the interaction with the target and can take any form. Reflection from a mirror at normal incidence, for instance, is described by and , while an idealized glint could be described by , where is the origin of the glint on the target, and is its effective area. Of primary interest here is reflection from a rough surface, which can be described by a pointwise random phase with . At first glance, it might appear that application of such a phase would eliminate implicit information of the optical configuration contained in Eq. (7): with , averages to zero. However, an interpretation of Eq. (7) in terms of a random walk in the complex plane reveals its significance.
We conceptualize the continuous target surface as a grid of discrete scatterers. Each scatterer is separated by a distance , occupies an area , and has a uniformly distributed random phase. This is equivalent to approximating Eq. (7) as a Riemann sum:
where , , is the location of the th scatterer, is the number of scatterers illuminated by the incident radiation; we have mapped the 2D coordinate system to a 1D array for convenience. Equation (8) is a sum over random phasors and, thus, can be interpreted as a random walk in the complex plane [11]. Typically, the transverse coherence length of optical phase fluctuations [12] far exceeds the correlation length of a rough surface [13]. Thus, we ignore the phase contributed by the incident field in the following discussion such that . Simulations presented below provide further justification for this.The magnitude of each step in the random walk is proportional to the intensity at a single location in the target plane, , while the direction of each step is determined by . The walk’s result is the field measured in the detector plane. For simplicity, we consider the uniform illumination of an incoherent reflector, corresponding to an isotropic, uniform random walk. This fixes all to a single value, , such that the expected intensity in the detector plane is given by , where the brackets denote the expected value.
Because is determined by the target, it cannot be modified, and the random walk will remain isotropic. However, by adjusting the outgoing beam’s phase, the intensity distribution on the target, i.e., the length of each step in the walk, can be modified. In particular, if the beam power, , is fixed, then , and . This proportionality demonstrates that, on average, an intensity increase at the detector point translates to an increase in the target plane intensity.
We continue by applying this analysis to focusing a laser beam through atmospheric turbulence onto a rough surface. Specifically, we simulate the optical configuration depicted in Fig. 1. A , collimated laser beam is initialized in the transmitter plane with a transverse Gaussian profile of spot size . Between the transmitter and the target, the beam evolves according to the steady-state paraxial wave equation with turbulence-induced refractive index fluctuations included through phase screens [14,15]. In the phase screen approximation, the beam acquires the accumulated phase distortions due to turbulence at discrete axial points along the propagation path, and is propagated in vacuum between these points. We use an analytic approximation of the Hill spectrum to characterize the distribution of turbulent scale sizes with an inner scale of 1 mm and outer scale of 1 m [3].
To simulate scattering from the rough surface at the target plane, we first apply a random phase uniformly distributed from zero to to the electric field amplitude at each grid point [11]. We then apply a circular filter in the Fourier domain that eliminates transverse wave numbers near the domain boundary. Propagation between the receiver and detector plane is modeled using a Fourier transform and appropriate scaling of the domain lengths based on the focal length of the lens.
As a demonstration of Eq. (7), and to verify the numerical model, we simulated propagation through 1000 realizations of the optical configuration shown in Fig. 1. The turbulent channel was 2.5 km long, and composed of 10 phase screens, each with a refractive index structure constant, , chosen randomly from a uniform distribution on the interval . Choosing randomly for each realization provides verification over a wide range of turbulence-induced beam distortions. The aperture function was set to a Gaussian, , with . Figure 2 displays scatter plots of the resulting left- and right-hand sides of Eq. (7) using the previously described normalization. Both the phase and amplitude predicted by the simulation are in excellent agreement with Eq. (7). We note that the simulation includes the turbulence phase contribution neglected in the random walk discussion above.
The random walk interpretation of Eq. (7) suggested a positive correlation between the focal and target intensities. Thus, a feedback loop where the focal intensity informs the phase imparted to the transmitted beam, should, on average, result in an increased intensity on target. In the remainder, we describe simulations of an adaptive optics implementation that does just that. The adaptive optics system consists of a phase modulator (Fig. 1) in the transmitter/receiver plane controlled by the stochastic parallel gradient descent algorithm (SPGD), which we return to below. The phase modulator is composed of square elements length on a side in a array. Each element can make piston phase changes. The elements are indexed by and , corresponding to the and dimensions, respectively, and are defined on the interval . For example, the indices , , and correspond to the bottom left, center, and top right elements, respectively.
We use the conventional stochastic parallel gradient descent (SPGD) algorithm and notation [16]. The SPGD algorithm is designed to iteratively increase a metric by applying random perturbations to all control parameters and calculating the gradient of the metric. Motivated by the preceding discussion, our metric is . The phases applied by each element of the phase modulator serve as the control parameters. In particular, the phase applied by element , at the end of iteration is defined as , calculated in three steps: , , and
where is randomly chosen as or for each element, is the magnitude of the perturbation, corresponds to the metric value resulting from , and is the gain coefficient.For the simulation, we chose the adaptive optics parameters , , and . The turbulent channel was 2.5 km in length with a . This is considered mild optical turbulence; we elaborate on the motivation for these parameters and limitations of the adaptive optics system below. The transmitted beam had clipped at diameter . The corresponding transfer function for the aperture and phase modulator during iteration is given by
where is defined as the Heaviside step function, and is the phase applied by the phase modulator. Simulations were conducted for 300 statistically independent turbulent channels. Each simulation completed 100 iterations of the SPGD phase correction algorithm.Figures 3(a) and 3(b) show the intensity profiles during iterations 1 and 100, respectively, where the correction algorithm was most effective, i.e., producing the highest maximum intensity on the target. In this instance, the maximum intensity during the first iteration is 1.7 due to minor scintillation effects, but a localized region of high intensity does not exist. After 100 iterations of the SPGD algorithm, the metric increased from to . The beam during iteration 100, displayed in Fig. 3(b), exhibits a single localized region of high intensity, 9.5 times the transmitted beam’s maximum intensity with approximately 10% of the transmitted power contained in a radius of 1 cm about the peak intensity. Out of the 300 simulations there were only nine instances where the correction algorithm did not increase the maximum intensity on the target. Figures 3(c) and 3(d) display the intensity profiles during iterations 1 and 100, respectively, for one such instance. In this simulation, the SPGD algorithm increased the metric from to , while the maximum intensity decreased from 2.6 to 2.1. Instead of a single, localized region of high intensity, there are multiple local intensity maxima. By chance, the incoherent sums for each of these maxima added constructively and resulted in an increased metric without an increased intensity on the target. In practice, the combination of a moving target with a finite photodetector exposure time would effectively perform an average and may mitigate such an occurrence.
Statistics over all 300 simulations are displayed in Fig. 4. Figures 4(a) and 4(b) display histograms of the maximum intensity and power in the bucket (PIB) on the target. The PIB is calculated as fractional power contained within a 1 cm radius bucket centered on the location of maximum intensity. Statistics obtained from intensity profiles during iterations 1 and 100 are plotted as the red and blue bars, respectively. Due to minor scintillation, the average maximum intensity during iteration 1 is 1.9 with a standard deviation of. 36. After 100 iterations of SPGD, the average maximum intensity is 3.5 with a standard deviation of 1.2. The same trend is seen in the PIB. The average PIB during iteration 1 is .027 with a standard deviation of .005, and the average PIB during iteration 100 is .045 with a standard deviation of .015.
In choosing the parameters for adaptive focusing based on Eq. (7), several conditions and limitations must be considered. First, there cannot be substantial intensity scintillation. Since our adaptive optics implementation only applies phase corrections, it cannot effectively correct for strong scintillation [17–19]. For a plane wave, the scintillation index is the Rytov variance, , and the condition for weak turbulence is . Recent research in combined amplitude and phase corrections may relax this condition [19]. Second, the dimension of the phase modulator elements must be less than the transverse coherence length, , where . Ideally a fast algorithm for correcting the wavefront would allow arbitrarily small phase modulator elements. However, with iterative algorithms, decreasing the element dimension can require decreasing the perturbation magnitude, , which increases the convergence time. Finally, iterative algorithms find local optima, which are not necessarily the ideal global optimum [16]. More sophisticated algorithms may offer a solution, but are a fundamental adaptive optics problem beyond the scope of this Letter. Working within these limits, we have demonstrated the derived relation can facilitate the formation of a localized region of high intensity on a remote, spatially incoherent target. The derived relation is quite general, relying entirely on reciprocity, making it suitable for applications requiring propagation through random media.
Funding
Office of Naval Research (ONR) (N000141211029).
Acknowledgment
The authors would like to thank J. Peñano, P. Sprangle, L. Andrews, and R. Phillips for fruitful discussions.
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