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SCIENCE REQUIREMENT |
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| Large Area Coverage |
Monitor lightning in the tropics, extra tropics to 50 degree latitude over both land and water
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Provide data sets from as many areas of the globe that will assure unbiased performance statistics; assure operations over calibration/validation sites;
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| High Detection Efficiency |
Estimate the total lighting activity of each storm |
Used for inferring convective activity, mixed phase precipitation, etc. |
| Low False Event Rates |
accurately detect only lightning events |
Less than 5% of total events
Minimize ground based processing
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| Measurement Sensitivity |
3.8 x 10-6 j m-2 um-1 sr-1 (preferred)
4.7 x 10-6 j m-2 um-1 sr-1 (acceptable)
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The sensitivity numbers include 6 dB of SNR margin. |
| Dynamic Range |
> 2 orders of magnitude |
After background subtraction, the system must maintain greater than 2 orders of magnitude dynamic range for lightning detection.
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| Spatial Resolution |
Identify individual convective cell |
8 km at nadir |
| Contiguous Observations |
continuous observation of the monitored area; |
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| Single Wavelength Operation |
Daytime lightning detection |
7774 A |
| Radiometric Measurement |
Determine lightning intensity |
measure to 10% accuracy |
| Continuing current |
Detect and quantize continuing current |
Do not update background during active pixel periods |
| Data compression |
High event rate throughput |
multiple dimension, adjacent pixel compression |
| Platform Attitude |
Earth viewing |
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| Command and Control |
Must be able to
- select subarray(s)
- adjust threshold
- select image area
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map 20 subregions to 16 RTEPs
preferred RTEP readout
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| Pointing Accuracy |
Locate lightning to specific cell |
110 microradians |
| Pointing Knowledge |
Locate lightning to specific cell |
40 microradians |
5.2. During Flight
The actual on-orbit performance will depend on the instrument performance and its calibration, the background scene stability, radiation effects, and source characteristics.
5.2.1. Ground Truth
Permanent ground validation sites will be established prior to launch. These sites will be used to validate instrument performance. Sites will likely include existing TRMM sites that are within the instrument field of view.
5.2.2. Field Campaigns
Intensive field campaigns will take place on a periodic basis to perform LMS validation and to investigate relationships between lightning and other convective parameters.
5.2.3 Navigation
Navigation will be verified using land marks identified from LMS images. Algorithms will be developed to compensate for identified pointing errors that occur as a function of the diurnal and seasonal cycles.
A.1. Lightning Instrument
A.1.1 LMS Measurement Approach
The LMS images a scene much like a television camera. However, because of the transient nature of lightning, its spectral characteristics, and the difficulty of daytime detection of lightning against brightly lit cloud backgrounds, actual data handling and processing is much different from that required by a simple imager. In order to achieve the performance goals required to meet the scientific objectives, the LMS combines many off-the-shelf and custom components in a unique configuration. A wide field of view telescope, combined with a large, narrow-band interference filter is focused on a high speed mosaic array focal plane. The signal is read out from the focal plane into real-time event processors (RTEP) for event detection and data compression. The resulting "lightning data only" signal is formatted, queued, and transmitted via the satellite to ground.
The specific characteristics of the sensor design result from the requirement
to detect weak lightning signals during the day. During the day, the background
illumination produced by sunlight reflecting from the tops of clouds is
much brighter than the illumination produced by lightning. Consequently,
the daytime lightning signals tend to be buried in the background noise,
and the only way to detect lightning during daytime is to implement techniques
that increase or maximize the lightning signal relative to this bright
background. These techniques take advantage of the significant differences
in the temporal, spatial, and spectral characteristics between the lightning
signal and the background noise. A combination of four methods will be
employed by the LMS for this purpose. First, spatial filtering is used
which matches the instantaneous field of view (IFOV) of each detector
element in the LMS focal plane array to the typical cloud-top area illuminated
by a lightning stroke (i.e., ~10 km). This results in an optimal sampling
of the lightning scene relative to the background illumination. Second,
spectral filtering is obtained by using a narrow-band interference filter
centered on a strong optical emission line (e.g., OI(1) at 777.4 nm) in
the lightning spectrum. This method further maximizes the lightning signal
relative to the reflected daylight background. Third, the LMS employs
temporal filtering which takes advantage of the difference in lightning
pulse duration which is on the order of 400 microseconds versus the background
illumination which tends to be constant on the time scale of seconds.
In an integrating sensor, such as the LMS, the integration time specifies
how long a particular pixel accumulates charge between readouts. The lightning
signal-to-noise ratio improves as the integration period approaches the
pulse duration. If, however, the integration period becomes too short,
the lightning signal tends to be split between successive frames which
actually decreases the signal-to-noise ratio. Since the median optical
lightning pulse width when viewed from above is 400 microseconds, an integration
time of 1 ms is most appropriate to minimize pulse splitting and maximize
lightning detectability. Present technological limitations require that
a 2 millisecond integration time be used in the LMS instrument design.
As demonstrated by the OTD and the LIS, this compromise does not seriously
degrade the sensor's performance.
Even with the three "filtering" approaches discussed above, the ratio of the background illumination to the lightning signal will often still exceed 100 to 1 at the focal plane. Therefore, a fourth technique, a modified frame-to-frame background subtraction, is implemented to remove the slowly varying background signal from the raw data coming off the LMS focal plane. A detailed discussion on the measurement approach proposed for the LMS is given in a later section of this document. Each real-time event processor generates an estimate of the background scene imaged at each pixel of its section of the focal plane array. This background scene is updated during each frame readout sequence and, at the same time, the background signal is compared with the off-the-focal-plane signal on a pixel-by-pixel basis. When the difference between these signals exceeds a selected threshold, the signal is identified as a lightning event and an event processing sequence is initiated. The implementation of this RTEP results in a 106 reduction in data rate requirements, while maintaining high detection efficiency for lightning events.
A.1.2 INSTRUMENT DESCRIPTION
The LMS will consist of a staring imager optimized to detect and locate lightning. An imaging system, a focal plane assembly, real-time event processors, a formatter, power supply, and interface electronics are the six major subsystems of the sensor. The imaging system is a fast f/1.2 telescope with a 12 cm aperture, and an 10 nm interference filter. The 5o x 5o LMS field of view must be restricted in order to minimize wavelength shifts through the interference filter. The focal plane assembly, (including a 700 x 560 pixel array, preamplifiers, multiplexers, and clock and drive electronics) provides an analog data stream of an appropriate amplitude to subsequent circuits. As noted earlier if, after background removal, the difference signal for a given pixel exceeds a threshold, that pixel is considered to contain an event. Subsequently, the event is time tagged, location tagged, background bin tagged, and passed to the satellite for transmission to the ground.
A.1.3 Imaging System
The imaging system includes an f/1.2, 11 cm diameter telescope and a 1 nm bandwidth interference filter. A broad-band blocking filter is placed on the front surface of the filter substrate in order to maximize the effectiveness of the narrow-band filter.
Because the bandpass of interference filters shifts to shorter wavelengths
for non-normal incidence, it is necessary to restrict the field of view
of the optics and use two telescopes to cover the required FOV. That is,
if the wavelength of interest is incident upon the filter at an angle
that shifts it beyond the filter bandpass, the signal will not be passed.
This problem is minimized by choosing a filter which passes the high wavelength
end of its bandpass at normal incidence. As the angle of incidence increases
to a maximum, the wavelength shifts down through the entire band pass
to the low wavelength end, allowing the full filter bandwidth to compensate
for the wavelength shift.
The filter temperature is controlled with an active thermal heating
system in order in insure minimal filter wavelength shift as a function
of temperature. Furthermore, the temperature control point can be adjusted
on orbit.
As noted previously, the RTEP detects weak lightning flashes from an intense, but slowly evolving background. The daytime background varies with sun angle, clouds, ground albedo, etc., and can reach in excess of 900,000 photo-electrons as compared to lightning produced signal electrons which may be as small as 6000 electrons. Typically lightning stroke will occur during a single integration frame producing a signal that is superimposed on top of the essentially constant background. The RTEP continuously averages the output from the focal plane over a number frames on a pixel-by-pixel basis in order to generate a background estimate. It then subtracts the average background estimate of each pixel from the current signal of the corresponding pixel.
The subtracted signal consists of shot noise fluctuating about zero with occasional peaks due to lightning events. When a peak exceeds the level of a variable threshold, it triggers comparator circuits and is processed by the rest of the electronics as a lightning event. The threshold must be set sufficiently high that false triggers are kept to a small percent of the total lightning rate. Clearly, the threshold must be higher during daytime when shot noise is dominated by the solar background
The components of the real-time event processor include a background signal estimator, a background remover, a lightning event thresholder, an event selector, and a signal identifier. Analog/digital hybrid processing is used in an unique way that takes advantage of the strengths of each technology in order to provide high processing rates while consuming minimal power. Much of the signal processing is performed in a pipeline fashion that maximizes throughput.
The background estimator (averager) and remover (subtraction) circuits combine to perform the functions of a time domain low pass filter. The signal coming off the focal plane is fed through a buffer and clipping stage in order to ensure that a strong lightning signal does not contaminate the background estimate. The signal is then multiplied by a fractional gain (B) and added to (1-B) times the previous background estimate for the same pixel. The inverse of the fractional gain is equivalent to the number of frames used in generating the background estimate and is analogous to setting the cutoff frequency in conventional frequency domain filters. Too high a fractional gain might permit lightning events to contaminate low background estimates and would increase the processing noise. Too low a fractional gain would not allow the background estimator to respond rapidly enough to changes in background intensity.
The proper operation of the background estimator requires that the background data are clocked through the estimator synchronously with the data being clock off the focal plane and that the number of discrete storage elements in the background memory is exactly the same as the number of pixels in the focal plane array. When data are properly synchronized, the signal appearing on the output of the delay line during a given clock cycle corresponds spatially to the signal being clocked off the focal plane. That is, it contains a history of what that specific pixel has measured over the last 1/B frames. These two signals are then subtracted using a difference amplifier in order to generate a difference signal. Since the original signal contains either background plus lightning or just background, the subtracted signal will be either a lightning signal, near zero or a false event.
The difference signal is then compared with the threshold level (which will be adaptive). If the signal exceeds the threshold level, a comparator triggers, which enables a switch and passes the lightning signal for further processing. In addition, the comparator output is encoded using a digital multiplexer in order to generate a row address which identifies the specific pixel that detected the lighting event. The digital outputs from the data processor represent the intensity of the lighting event and the location where the lightning occurred. These signals are then forwarded to encoding electronics in which the data are formatted into a digital bit stream and sent to the spacecraft. Experience from OTD and LIS have demonstrated that it is not necessary to remove all the false events with the RTEP. We have found that it is relatively straight forward to filter out the bad events via ground-based processing since the true lightning events have much different characteristics. The main function of the on-board processing is to capture all the lightning events and to reduce the number of false events to a manageable number that can be handled by the telemetry system.
The mapping of 20 subregions to 16 RTEPs should allow for the uninterrupted
observations of the continental United States under the conditions of
spacecraft yaw flips and one RTEP failure. This may be best accomplished
by allowing each RTEP to be mapped to one of two subregions.
After gaining on-orbit experience with the LMS, it may prove desirable to implement additional on-board signal processing. A forty percent reserve of processor resources must be preserved to support this requirement. The driver for this requirement would be improved real time data dissemination in support of operations. This level of signal processing would be implemented in software utilizing the LMS microprocessors. In addition, data record configuration options should allow for inclusion of event count and event amplitude summaries. A capability for selecting certain subregions for preferred event detection is also required. This allows full event rates in the preferred subregions at the expense of possibly missing event in other subregions.
The LMS requires power and data resources from the satellite bus. The packaging of the instrument will be driven by its location on the spacecraft, its field of view requirements, its need for passive thermal control and by the specific services provided by the bus. These issues require a detailed accommodation study to resolve. However since LMS is a small, lightweight sensor, it should be relatively easy to accommodate on the spacecraft with the main issue being heat dissipation and maintenance of pointing stability and knowledge.