1. Introduction
Optical array probes (OAP) mounted on research aircraft are used to characterize the shape, size, and concentration of large cloud particles during flight. Such probes use a 1D linear array to capture the occultation of a laser beam by cloud particles (Knollenberg 1981). Typical probe models process each detector in the array to report a shaded (digital zero) or not-shaded (digital 1) state based on a predefined detector threshold. The digital state of each detector channel is latched in at regular intervals and a 2D 1-bit image of the particle’s shadow is recorded. An example of such 2D cloud (2D-C) images captured by a probe with 25-μm resolution during the High-Performance Instrumented Airborne Platform for Environmental Research (HIAPER) Pole-to-Pole Observations 2 (HIPPO-2) is shown in Fig. 1 (Earth Observing Laboratory 2011).

2D-C images of ice particles at 25-μm resolution during HIPPO-2, research flight 6, at approximately 0110 UTC.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

2D-C images of ice particles at 25-μm resolution during HIPPO-2, research flight 6, at approximately 0110 UTC.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
2D-C images of ice particles at 25-μm resolution during HIPPO-2, research flight 6, at approximately 0110 UTC.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
This observational technique has the benefit of recording data independent of particle shape, but the effective sample volume of the probe depends on the particle size. Small particles have a smaller effective sample volume than that dictated by the probe arm separation. This can be beneficial because it allows the probe to operate over a large concentration regime. The probe is most sensitive to larger particles, which are typically found in low concentration, and much less sensitive to small particles, which are typically found in high concentration. Conversely, this fact requires that one accurately know the particle size and corresponding sample volume. Thus, the size-dependent sample volume of OAPs can represent a source of error in size-resolved concentration estimates.
The size-dependent sample volume of an OAP depends at least partly on the physical characteristics of the probes. This includes the detector response time characteristics, which were the subject of analysis by Baumgardner and Korolev (1997) and Jensen and Granek (2002). Those works focused on the effect of a 0.4-μs time constant on the accuracy of the Particle Measuring Systems (PMS) 260X probe, but they do not detail whether or how the response characteristic is determined. In Lawson et al. (2006), a response time constant is reported for the SPEC 2D stereo (2D-S) probe, which is measured using a high-bandwidth laser, but again it is not clear whether the assumed exponential waveform is verified. Finally, in Strapp et al. (2001) the PMS OAP-2DC response characteristics were measured, including a direct capture of the response waveform published in the manuscript. The assumed exponential function was shown to reflect the actual data after correcting for the modulation signal’s limited bandwidth. These results were obtained for much slower detectors than what we currently employ in our instruments, and factors that we find to be significant may have been negligible in systems with slower response.
At NCAR, the use of these probes on the NSF Gulfstream V (GV), which operates at high airspeeds (greater than 200 m s−1), makes the temporal response characteristics of our OAPs increasingly important for understanding their sample volumes. There is a need to characterize the detector response to better determine the sample volume and to understand realistic instrument capability. In particular, particle size and concentration measurements with a radius in the 20–100-μm (drizzle drop) size range have been scientifically desirable but difficult to measure with OAPs. Drops in this size range are believed to be important due to their potential effect on the lifetime of warm shallow clouds (Albrecht 1989). In this small size regime, the probes are increasingly sensitive to the physical characteristics of the probe. In an effort to better understand our OAP performance, we have developed a method for characterizing the response time of the detector system, starting with an optical input on the detector and measuring the corresponding digital output. In this way, the complete detection system is included in the analysis, and we are able to produce estimates of the detector system impulse response for inclusion in our OAP instrument models.
In this work we detail the method for acquiring OAP detector response data and its subsequent analysis. Section 2 contains a method for directly measuring the detector response characteristics from optical input to digital output of a Fast-2D detector board. Using a high-bandwidth (100 MHz) digital diode laser, we measure the characteristic step response of the detector circuit, including the digitizer (comparator). This is done by measuring the comparator transition times as we scan the comparator reference voltage by adjusting the illuminating laser duty cycle. We then compare these measurements to the minimum detectable pulse duration. Once the electronic response characteristics are determined, we apply the results to a model of a 2D probe in section 3 to estimate the size-dependent sample volume’s sensitivity to variations in the probe’s detector response time. Finally, a summary is given in section 4.
2. Measurements
The Fast-2D board [model ABD-0001, also called the cloud imaging probe (CIP) mono diode array] is manufactured by Droplet Measurement Technologies (DMT, Boulder, Colorado) and it consists of a linear photodiode array, where each photodiode current is converted to a voltage through a transimpedance amplifier. That voltage is then further amplified and drives a comparator circuit that generates a 1-bit not-shaded (digital 1) or shaded (digital 0) output state for the photodiode. A simplified schematic of the Fast-2D circuit is shown in Fig. 2.

Schematic description of the detection circuit on the Fast-2D board. A photodiode drives an analog amplifier stage that serves as the input to a comparator. The comparator outputs a digital zero if the amplifier voltage falls below 50% of the average amplifier voltage (indicating the photodiode is shaded). The LP filter refers to a low-pass filter with a cutoff frequency of approximately 250 Hz.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Schematic description of the detection circuit on the Fast-2D board. A photodiode drives an analog amplifier stage that serves as the input to a comparator. The comparator outputs a digital zero if the amplifier voltage falls below 50% of the average amplifier voltage (indicating the photodiode is shaded). The LP filter refers to a low-pass filter with a cutoff frequency of approximately 250 Hz.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Schematic description of the detection circuit on the Fast-2D board. A photodiode drives an analog amplifier stage that serves as the input to a comparator. The comparator outputs a digital zero if the amplifier voltage falls below 50% of the average amplifier voltage (indicating the photodiode is shaded). The LP filter refers to a low-pass filter with a cutoff frequency of approximately 250 Hz.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1









Approximate shading required to change a comparator output from not shaded to shaded for the standard output (blue) designed for 50% shading, and the DOF output (green) designed for 67% shading. The required shading always exceeds the design value (dashed lines) due to the bias effect of hysteresis in the comparator. They asymptotically approach the design value as the average amplifier voltage increases. The Fast-2D amplifier saturates just below 4 V.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Approximate shading required to change a comparator output from not shaded to shaded for the standard output (blue) designed for 50% shading, and the DOF output (green) designed for 67% shading. The required shading always exceeds the design value (dashed lines) due to the bias effect of hysteresis in the comparator. They asymptotically approach the design value as the average amplifier voltage increases. The Fast-2D amplifier saturates just below 4 V.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Approximate shading required to change a comparator output from not shaded to shaded for the standard output (blue) designed for 50% shading, and the DOF output (green) designed for 67% shading. The required shading always exceeds the design value (dashed lines) due to the bias effect of hysteresis in the comparator. They asymptotically approach the design value as the average amplifier voltage increases. The Fast-2D amplifier saturates just below 4 V.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Each detector circuit has a corresponding DOF circuit that is identical to the standard comparator circuit, except that the comparator threshold is theoretically set to 67% shading (the amplifier output is split into the two comparator circuits). A particle is accepted as “in the sample volume” if at least one DOF comparator is triggered by the particle. In addition to the standard comparator output, Fig. 3 also shows the required shading for the DOF flag as a function of average amplifier voltage.
A likely point for characterizing the response time of the detector circuit is the analog test point immediately preceding the comparator circuit in Fig. 2; however, this omits the comparator response characteristics. The resistor
We have two measurements for assessing the dynamics of the detector system on the Fast-2D board. The test setup used for both measurements is shown in Fig. 4. A high bandwidth (100-MHz or 2-ns rise/fall time) digital diode laser (Newport LQD660-110C) is modulated between (mostly) on and (very briefly) off states. The laser is collimated by a 30-mm lens and passed through a half-wave plate (HWP) and polarizing beam splitter (PBS), where one port is directed onto a high-bandwidth photodiode (Thorlabs DET10A with 1-ns rise time at 50Ω load) as a time reference and monitor for the laser signal. The laser pulse demonstrates a fall time of approximately 3 ns when monitored with the DET10A. The HWP is used to control the split in laser power between the two PBS ports. The light exiting the other PBS port is directed onto the Fast-2D detector array through a periscope (not pictured). We then monitor the analog test point on the Fast-2D board to determine the steady-state voltage when the laser is on and off, and we make sure the input signal is not saturating any of the detection electronics. We monitor the output state of the comparator to determine whether the board is responding to the input pulse (see the next subsection) and to determine the time at which the voltage waveform crosses the threshold voltage (see section 2b). Table 1 summarizes all the measured and derived variables for characterization of the Fast-2D board.

Test setup for measuring the response time characteristics of the Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Test setup for measuring the response time characteristics of the Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Test setup for measuring the response time characteristics of the Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Measured and derived variables and their sources.


a. Minimum pulse width
In the first measurement, a diode laser illuminates the photodiode array. The laser is normally on except for very short periods where the laser is turned off to simulate shading from a particle passing through the beam. We progressively reduce the duration where the laser is off until the detection circuit does not respond fast enough to cause a change in state in the digital output. Contributions of zero-mean noise will blur this exact boundary, so we estimate the fraction of input pulses that result in a change in comparator output state and report here the 50% point (ideally where the limit would be if noise were absent). The histogram in Fig. 5 shows the distribution of minimum response times for all 64 channels on a Fast-2D board. The sizable spread would seem to suggest that there is significant variation in the response characteristics of the different detection channels. Furthermore, it seems to suggest the board does not meet its 50-ns time constant specification. We will show in the next section that an unexpected slow decay term is having a detrimental effect on the detector performance.

Histogram of the minimum detectable input pulse width for all 64 channels on a Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Histogram of the minimum detectable input pulse width for all 64 channels on a Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Histogram of the minimum detectable input pulse width for all 64 channels on a Fast-2D board.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
b. Total voltage waveform
In our second test, we measure an effective voltage-versus-time waveform for a case when the laser is initially on and turned off very rapidly (with a bandwidth of 100 MHz, the laser has a fall time on the order of 2 ns). This step-down input is functionally described as




The waveform resulting from a step-down input appears to have two different components associated with it (see data plotted in Fig. 6). One is clearly the result of the electronic response time, which is an exponential with a time constant on the order of 50 ns. The other dynamic term has a very slow response characteristic and does not conform well with an exponential decay function. The total detected waveform is the sum of the two decay terms.

The observed and fit decay function of the total detector system on the Fast-2D board. The fit, described by Eq. (3), includes an exponential term (blue) attributed to the electronic response of the system and a slow decay term (red). The top dashed line indicates the steady-state voltage
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

The observed and fit decay function of the total detector system on the Fast-2D board. The fit, described by Eq. (3), includes an exponential term (blue) attributed to the electronic response of the system and a slow decay term (red). The top dashed line indicates the steady-state voltage
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
The observed and fit decay function of the total detector system on the Fast-2D board. The fit, described by Eq. (3), includes an exponential term (blue) attributed to the electronic response of the system and a slow decay term (red). The top dashed line indicates the steady-state voltage
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
The physical effect responsible for the slow decay remains unclear. Capacitive coupling was considered, but we can change the amount of slow decay in the waveform by adjusting the laser angle of incidence (near-normal incidence significantly reduces the amplitude of the slow decay).
The slow term could be the result of scattering between a reflective mask over the photodiode array and the matte white surface on which the diode array is mounted. However, the relative separation between the two surfaces is on the order of millimeters, so a decay function on the order of 1 μs would have to experience approximately 300 000 reflections and require a surface reflectivity larger than 0.999 997. Also, the decay function of most scattering is expected to conform to an exponential form.
Finally, it may be possible the laser excites electron-hole pairs in an inactive region of the detector and the carriers have very slow diffusion rates. If these regions are near the edges of the photodiode, it might explain the dependence on the angle of incidence. Whatever the physical cause of the slow decay function, it remains a significant factor in the characterization and analysis of the detector system of the Fast-2D.
We did not observe this slow decay term on the DET10A that was monitoring the laser optical output, so we are confident that it is an attribute of the 2D board and not an artifact of the test equipment.



















An example of the fit waveform is shown in Fig. 6. We fit Eq. (3) to all 64 detector channels of a Fast-2D board. Table 2 contains a summary of the fit parameters from Eq. (3). All amplitude terms in Table 2 are normalized (except
A scatterplot of the electronic time constant versus slow fraction is shown as blue dots in Fig. 7. It is important to note that the electronic time constant is independent of the slow fraction. A poor fit function would likely couple these two terms. For comparison, Fig. 7 also shows the corresponding minimum detectable pulse widths described in the previous section. These pulse widths tend to be significantly larger than the electronic time constants and show a clear correlation with the slow fraction. This is expected, because as the slow fraction increases it will dominate the decay waveform and the effective response time of the system increases.

Plot of the estimated electronic time constants (blue dots) and the measured minimum detectable pulse widths (red x’s) vs slow fraction for each photodiode channel. The electronic time constants are independent of the slow fraction and well centered around the design response time. The minimum detectable pulse widths are impacted by the amplitude of the slow decay term in the detected signal, which significantly slows the overall response of the detection system.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Plot of the estimated electronic time constants (blue dots) and the measured minimum detectable pulse widths (red x’s) vs slow fraction for each photodiode channel. The electronic time constants are independent of the slow fraction and well centered around the design response time. The minimum detectable pulse widths are impacted by the amplitude of the slow decay term in the detected signal, which significantly slows the overall response of the detection system.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Plot of the estimated electronic time constants (blue dots) and the measured minimum detectable pulse widths (red x’s) vs slow fraction for each photodiode channel. The electronic time constants are independent of the slow fraction and well centered around the design response time. The minimum detectable pulse widths are impacted by the amplitude of the slow decay term in the detected signal, which significantly slows the overall response of the detection system.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Our observations of the Fast-2D detector system (optical input to digital output) did not significantly differ from the response characteristics we would have obtained from analyzing the amplifier output at the analog test point. However, as the analog front end of the detection system is pushed to faster response times, the response characteristics of the digitizer will likely become more significant. The analysis shown here is important, because the response characteristics of a digitizer can be difficult to measure directly. A complete analysis should include all of the analog components, including the digitizer.
We have found that the electronic time constant of our Fast-2D boards is near its design specification of 50 ns. However, the effective response time of the detector is slower due to an additional response characteristic. Were the slow decay term not a factor, we would expect the minimum detectable pulse width to be less than the electronic time constant. Instead, we typically observed minimum pulse widths in the range of 70–150 ns.








Setup for measuring the scattering fraction as a function of the angle of incidence. The bright red arrow indicates light directed onto the detector. The darker red arrow is light reflected by the mask over the detector.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Setup for measuring the scattering fraction as a function of the angle of incidence. The bright red arrow indicates light directed onto the detector. The darker red arrow is light reflected by the mask over the detector.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Setup for measuring the scattering fraction as a function of the angle of incidence. The bright red arrow indicates light directed onto the detector. The darker red arrow is light reflected by the mask over the detector.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Plot of the estimated slow fraction as a function of the angle of incidence. (left) The raw measurements are taken over ±0.3° and are substantially scattered for the different channels. (right) An optimization routine is used to adjust the offset angles of each channel to obtain a quadratic function resulting in the scatterplot shown here (offsets used are given in Table 3). The variation in offset angles between channels may be the result of the small misalignment between the mask and detector on the Fast-2D.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Plot of the estimated slow fraction as a function of the angle of incidence. (left) The raw measurements are taken over ±0.3° and are substantially scattered for the different channels. (right) An optimization routine is used to adjust the offset angles of each channel to obtain a quadratic function resulting in the scatterplot shown here (offsets used are given in Table 3). The variation in offset angles between channels may be the result of the small misalignment between the mask and detector on the Fast-2D.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Plot of the estimated slow fraction as a function of the angle of incidence. (left) The raw measurements are taken over ±0.3° and are substantially scattered for the different channels. (right) An optimization routine is used to adjust the offset angles of each channel to obtain a quadratic function resulting in the scatterplot shown here (offsets used are given in Table 3). The variation in offset angles between channels may be the result of the small misalignment between the mask and detector on the Fast-2D.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
In previous investigations we had found that adjacent even and odd array photodiodes seemed to have different angular sensitivity, suggesting that the mask over the detector array was slightly offset. In addition to the difference in angular sensitivity, it also seems that the scattering fraction has offsets that may be a similar result of a mask offset. Channels 17, 18, and 24 all seem to show a minimum in scattering fraction but at different angles of incidence. Meanwhile, channel 45 appears to be significantly offset from the minimum. All of the data were taken at the same absolute angles of incidence (shown in the left plot of Fig. 9). We fit the data to a quadratic function and allow the optimizer to adjust the angular offsets of each channel. This provides a more coherent picture of the angle of incidence versus the scattering fraction shown in the right plot of Fig. 9. The angle offsets of the tested channels are given in Table 3.
Offset angles of four channels examined for slow fraction dependence on the angle of incidence.


The Fast-2D scattering fraction seems to be quite sensitive to the angle of incidence. To obtain a scattering fraction of less than 0.1, it would seem that there is about a 1° tolerance in the angle of incidence. This assumes that the detected sensitivity is symmetric, which we could not confirm. The test setup cannot measure a wide range of incidence angles (limited to approximately ±0.3°), so we are subject to the alignment of the detector mask on this particular board. Thus, these results are not fully conclusive with regard to detector tolerancing, but it does suggest that the boards are quite sensitive in at least one incidence direction.
We should not expect all detectors, even on the same Fast-2D card, to have the same slow fraction. It would appear that slight deviations in mask alignment to the detector determine where the incident beam lies on the angle of incidence versus the slow fraction curve. The angle of incidence that obtains a small slow fraction in one channel is very likely suboptimal for another channel.
3. Response time effect on probe sample volume
The step response characteristics measured in the sections above suggest the electronic response of the detection system is quite fast, but the slow decay term may significantly slow the overall detection system and adversely impact the instrument’s ability to measure small particles. To better understand the effects of response time, we use the results reported above in a 2D probe simulation.
a. Simulation description
The 2D probe simulation used here is largely composed of a diffraction model and includes a number of prior determined characteristics. It models the incident wave front as an elliptical Gaussian beam with 0.2-mrad vertical divergence and 0.6-mrad horizontal divergence based on laboratory measurements of the beam. Prior published OAP 2D simulations have been limited to plane-parallel waves. It also includes the optical receiver point spread function (PSF), which has been characterized as a 10-μm-diameter (null to null) diffraction-limited spot (or Airy disk). The PSF represents the smallest resolvable feature and is the spatial analog to the impulse response of a dynamic system. The PSF results in blurring of an image such that features smaller than the PSF typically cannot be resolved. Prior published OAP simulations do not include the PSF, which may be important in assessing the sample volume of small particles consisting of only a few pixels.









This method of propagating waves is practically similar to the Fresnel convolutions performed in Korolev et al. (1991). The Fourier transform method tends to be faster when Fresnel convolution kernels are near the same size as the total grid area, but it has the drawback of aliasing (where diffracted patterns that exit the edge of the modeled area wrap around).
The initial simulation runs at a much smaller spatial grid spacing than what is actually measured by the probe. Optical diffraction calculations are performed on a grid with a spacing of 1.5625 μm. The grid spacing details are included in the simulation table.

































The definition for an elliptical Gaussian beam provided above assumes the major and minor axes are aligned to x and y coordinates, respectively. Rotating the axes can be accomplished by substituting a rotated coordinate system into the above-mentioned definitions.
























The photodiode spacing on the instrument








Examples of a particle through the stages of analysis are shown in Fig. 10, where

An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
An example of the simulation output for a 137.5-μm particle at
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Simulation of the effects of slow fraction (
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Simulation of the effects of slow fraction (
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Simulation of the effects of slow fraction (
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
In this analysis we use the DOF flag (requires 67% shading) to determine whether a particle is in the probe sample volume. If at least one pixel triggers the DOF flag, we count the particle as being in the sample volume. We then count the number of particles in the sample volume and divide by the total number of particles simulated to provide the probability of detection. Note that we do not require the particle be sized correctly, as this will depend on the specific OAP processing code. To determine the sample area of a particular particle size, we multiply the probability of detection by the total simulated area of the particles. The parameters used for the 25-μm Fast 2D-C simulation are described in Table 4.
Simulation parameters for sample volume estimates.


b. Simulation results
The sample area as a function of particle size is shown in Fig. 13 for different slow fractions. These slow fractions correspond to the range of values observed during the initial detector characterization. The black line in the figure is the case where there are no response time effects in the probe. For comparison, the waveforms of those impulse responses are shown in Fig. 14.

Sample area of the 25-μm Fast 2D-C as a function of particle diameter for different slow fractions. The black line indicates the sample area if there is no response time effect in the probe. The near-horizontal lines in the upper-right corner correspond to the mechanical limitations due to the fixed distance between probe arms. The curves left of that region are where optical and electrical characteristics of the probe determine the particle sample area.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Sample area of the 25-μm Fast 2D-C as a function of particle diameter for different slow fractions. The black line indicates the sample area if there is no response time effect in the probe. The near-horizontal lines in the upper-right corner correspond to the mechanical limitations due to the fixed distance between probe arms. The curves left of that region are where optical and electrical characteristics of the probe determine the particle sample area.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Sample area of the 25-μm Fast 2D-C as a function of particle diameter for different slow fractions. The black line indicates the sample area if there is no response time effect in the probe. The near-horizontal lines in the upper-right corner correspond to the mechanical limitations due to the fixed distance between probe arms. The curves left of that region are where optical and electrical characteristics of the probe determine the particle sample area.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Impulse responses (with maximum value normalized to one) for the slow fractions shown in Fig. 13.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Impulse responses (with maximum value normalized to one) for the slow fractions shown in Fig. 13.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Impulse responses (with maximum value normalized to one) for the slow fractions shown in Fig. 13.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
As the amount of energy in the slow decay term increases, it can have a significant effect on particle sample volume. Figure 15 shows the fractional difference in sample volume compared to the case where response time is not included in the simulation. In this case the slow fractions used are more realistic for operational 2D probes with values between 0 and 0.1. Figure 15 shows the significant challenge in estimating the sample area (and therefore particle concentrations), particularly at small sizes.

Fractional difference in the sample area for slow fractions between 0 and 0.1 relative to a probe with no response time effects.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Fractional difference in the sample area for slow fractions between 0 and 0.1 relative to a probe with no response time effects.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Fractional difference in the sample area for slow fractions between 0 and 0.1 relative to a probe with no response time effects.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
We expand the simulation of our 25-μm 2D-C probe to include airspeeds from 80 to 250 m s−1 with slow fractions between 0 and 0.1. We calculate the mean sample area as a function of particle diameter and airspeed, and the corresponding fractional spread in sample area (

Sample area (surface height) and fractional uncertainty in the sample area due to uncertainty in slow fraction (color) as a function of particle diameter and airspeed. Note the color axis is logarithmic.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1

Sample area (surface height) and fractional uncertainty in the sample area due to uncertainty in slow fraction (color) as a function of particle diameter and airspeed. Note the color axis is logarithmic.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
Sample area (surface height) and fractional uncertainty in the sample area due to uncertainty in slow fraction (color) as a function of particle diameter and airspeed. Note the color axis is logarithmic.
Citation: Journal of Atmospheric and Oceanic Technology 33, 12; 10.1175/JTECH-D-16-0062.1
The fractional uncertainty due to slow fraction will add in quadrature with other fractional uncertainty terms (e.g., sizing error, Poisson statistics, and any sample volume uncertainty arising from other unknowns in the probe operation). This means the error shown in Fig. 16 represents a base fractional uncertainty in particle concentration. While the results reported here raise some basic concerns about sizing particles in the smallest size bins, it also offers some assurance that the error in particle concentration caused by response time uncertainty is less than 10% for particles larger than the third bin (diameter of 87.5 μm and larger). Furthermore, the uncertainty due to slow fraction is not fundamental. If the slow fraction could be accurately determined for each individual channel on a specific probe, and we were confident the slow fractions would not change during flight, then the effects could be accounted for in the sample volume estimate. At this time, this does not seem practical because the analysis should include the probe’s illuminating laser, which does not currently have sufficient bandwidth for this analysis.
4. Conclusions
The response time characteristics of OAP detectors are known to have an impact on the accuracy of derived cloud and precipitation particle concentrations. While the effect of time constants has been discussed in other works, we have described a detailed method for characterizing the response behavior of the Fast-2D detector board. This analysis method includes the total detector system, from optical input to digitization, and includes a careful study of the observed waveforms.
We found that the electronic time constant of the Fast-2D is near its specified value of 50 ns. Where previously we have assumed that the electronic response time is the most important characteristic, we have found that an additional slow decay term appears to play a significant role in limiting the overall detection system bandwidth. We are able to adjust the amplitude of the slow decay term by adjusting the laser alignment to the detector board, but even at very near-normal incidence, typical slow fractions are between 0 and 0.1. This results in a spread of sample volume estimates ranging from less than 1% for particles larger than 150 μm to approximately 10% in the smallest size bins. To better constrain the spread in slow fraction across all channels on a board, the mask alignment to the photodiode array is critical.
Given the specific outcome of this work, the optical array probe community should be cautious about assuming their probe’s detection bandwidth is dictated solely by electronic circuit designs. Furthermore, instrument designers should be cognizant of other physical effects in the entire probe detection system (such as capacitive coupling, scattering, semiconductor detector response characteristics, and mask-to-photodiode array alignment). The effects of additional slow decay terms are of increasing concern for the design of state-of-the-art OAP components, since high-speed electronics cannot overcome bandwidth limitations imposed by other physical effects.
While there is considerable scientific motivation to push OAPs to characterize particles at smaller size ranges (10–100 μm), this work further emphasizes how small effects can have a significant impact on the performance of an OAP in this particle size range. Details that are insignificant at larger sizes can become dominating error sources in the smaller regimes. In this specific case we find there are previously unconsidered physical effects influencing the performance of the probe. We want to emphasize the importance of including physical effects not conventionally considered in OAP literature for OAP simulation, data analysis, and design in the small particle size range.
Finally, this work details only one piece of 2D probe characterization. Several other probe effects remain to be considered or ruled out in optical probe characterization. Comparator hysteresis, described briefly here, will likely cause the sample volume to have some dependence on the mean detector signal. The incident laser wave front, optical system PSF, and optical aberrations may impact the size-dependent sample volume and help explain some of the discrepancies in the depth-of-field (DOF) constant usually used to estimate the probe’s sample area. For a total probe characterization, a model using these (and possibly other) individual characterizations should be able to reproduce end-to-end test results [such as high-speed spinning disks or optical fiber described in Lawson et al. (2006)]. This validation process is essential, as the failure to obtain agreement indicates additional missing characterizations or possible mischaracterization of a component.
Acknowledgments
The authors thank Aaron Bansemer for providing exceptional feedback on the presentation and content of this work.
REFERENCES
Albrecht, B. A., 1989: Aerosols, cloud microphysics and fractional cloudiness. Science, 245, 1227–1230, doi:10.1126/science.245.4923.1227.
Baumgardner, D., and Korolev A. , 1997: Airspeed corrections for optical array probe sample volumes. J. Atmos. Oceanic Technol., 14, 1224–1229, doi:10.1175/1520-0426(1997)014<1224:ACFOAP>2.0.CO;2.
Earth Observing Laboratory, 2011: PMS-2D two-dimensional cloud probe data, version 1.0. UCAR/NCAR, accessed 16 January 2016, doi:10.5065/D6K935RC.
Goodman, J. W., 2005: Introduction to Fourier Optics. 3rd ed. Roberts & Company, 491 pp.
Jensen, J., and Granek H. , 2002: Optoelectronic simulation of the PMS 260X optical array probe and applications to drizzle in a marine stratocumulus. J. Atmos. Oceanic Technol., 19, 568–585, doi:10.1175/1520-0426(2002)019<0568:OSOTPO>2.0.CO;2.
Knollenberg, R. G., 1981: Techniques for probing cloudmicrostructure. Clouds: Their Formation, Optical Properties, and Effects, P. V. Hobbs and A. Deepak, Eds., Academic Press, 15–91.
Korolev, A. V., Kuznetsov S. V. , Makarov Y. E. , and Novikov V. S. , 1991: Evaluation of measurements of particle size and sample area from optical array probes. J. Atmos. Oceanic Technol., 8, 514–522, doi:10.1175/1520-0426(1991)008<0514:EOMOPS>2.0.CO;2.
Lawson, R. P., O’Connor D. , Zmarzly P. , Weaver K. , Baker B. , Mo Q. , and Jonsson H. , 2006: The 2D-S (stereo) probe: Design and preliminary tests of a new airborne, high-speed, high-resolution particle imaging probe. J. Atmos. Oceanic Technol., 23, 1462–1477, doi:10.1175/JTECH1927.1.
Strapp, J. W., Albers F. , Reuter A. , Korolev A. V. , Maixner U. , Rashke E. , and Vukovic Z. , 2001: Laboratory measurements of the response of a PMS OAP-2DC. J. Atmos. Oceanic Technol., 18, 1150–1170, doi:10.1175/1520-0426(2001)018<1150:LMOTRO>2.0.CO;2.
Yariv, A., and Yeh P. , 2007: Photonics: Optical Electronics in Modern Communications. 6th ed. Oxford University Press, 836 pp.