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The Mars Lidar Simulation Model (MLSM) Differential Absorption Lidar Systems |
The LSM simulates the performance of coherent lidars as space-based remote sensors CO2 concentration with an emphasis upon a realistic representation of the atmosphere along individual line of sights. The MLSM version 1.0 optical property data bases supports DIAL wavelengths for a 2.053472 mm off line channel and 2.053208 - 2.0531997 mm on line channels.
Coherent DIAL Signal Processing Model
The coherent wide band SNR equation used in for the coherent DWL is used for the coherent DIAL and is defined as
SNRW = (p×h1×h2×h3×h4×h5×J×D2×l2 ß×e-2óa(r)dr)/(8×hn×2×Vmax×R2)
where
h
1 - heterodyne quantum efficiencyh
2 - transmit optical efficiencyh
3 - receive optical efficiencyh4 - mixing efficiency
h
5 - coherent system marginJ
- fundamental laser energy per pulse (Joules)D
- mirror diameter (m)ß - backscatter (m-1 sr-1)
e-2óa(r)dr
- 2 way attenuationhn
- photon energy (J)R
- slant range (m)l
- laser wavelength (m)Vmax - signal velocity bandwidth. [Set to 1.0 for DIAL simulation]
The MLSM simulates the user's prescribed DIAL system compared to what the same DIAL system would measure for a chosen Martian standard atmosphere. The current standard atmosphere is considered to be the median atmosphere. The measured and the standard atmosphere wideband signal to noises are accumulated for the on and off channels as follows

Ponm = (S SNRwonm(z))/N Poffm = (S SNRwoffm(z))/N
Pons = (S SNRwons(z))/N Poffs = (S SNRwoffs(z))/N
where
SNRwonm - measured signal to noise for range gate, on channel
SNRwons - standard atmosphere signal to noise for range gate, on channel
SNRwoffm - measured signal to noise for range gate, off channel
SNRwoffs - standard atmosphere signal to noise for range gate, off channel
Ponm - accumulated measured signal for on channel
Pons - accumulated standard atmosphere signal for on channel
Poffm - accumulated measured signal for off channel
Poffs - accumulated standard atmosphere signal for off channel
N - Number of samples in the grid volume.
T and B - top and bottom of the accumulation layer, respectively.
The MLSM output product is the vertical profile of the density of the CO2 atmosphere to the density of the CO2 Standard Atmosphere.

rCO2m - density DIAL measurement product of CO2
rCO2s - density DIAL Standard Atmosphere product of CO2
NASA/LaRC and SWA developed a first attempt representation of the DIAL CO2 measurement error for the MLSM. This equation is ongoing review. Using the parameter, PHI, from the coherent lidar model the MLSM estimates the percent error in making a CO2 concentration as follows.
The effective wideband SNR (db) is computed by accumulating all the samples in an user's defined grid volume.
SNRWeff = 10×log10( (S(SNRWi)2)0.5)
The number of data samples per LOS range gate is given as
m = (2.0 * d * 2.0 * Vmax) / (c * l * 1E-6)
where
l
- wavelength (m)Vmax
- maximum velocity measuredc - speed of light (m/s)
d - range gate (m).
Thus the effective photons per LOS range gate is
f = m * SNRWeff.

Questions on the DIAL Signal Processing Models mailto: Dave Emmitt or Grady Koch
Last Updated: 02/07/2007