TES deconvolution cookbook
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pnl_motion = 1 (min) to 2 (max). | pnl_motion = 1 (min) to 2 (max). | ||
+ | * Limit spacecraft ''ocks'' | ||
+ | ock (min) = 1583. | ||
− | |||
− | |||
− | |||
This is the start of the science phase, same as orbit 0. | This is the start of the science phase, same as orbit 0. | ||
− | ock (max) = 7000. | + | ock (max) = 7000. |
For ocks above 7000, the TES detectors sometimes exhibit an instrumental error (the "glitch") that results in a reversal of the dust absorption near 1100 wavenumbers, creating a broad peak with random direction (peak or trough) and amplitude in the spectra centered around 1000 wn, and extending between 900-1100 wn. This is most likely caused by internal motion within the spacecraft affecting the interferometer. The glitch can be somewhat compensated for by averaging many icks from the same ock, but this isn't recommended for most applications. Bolometer/albedo data is not affected by the glitch. | For ocks above 7000, the TES detectors sometimes exhibit an instrumental error (the "glitch") that results in a reversal of the dust absorption near 1100 wavenumbers, creating a broad peak with random direction (peak or trough) and amplitude in the spectra centered around 1000 wn, and extending between 900-1100 wn. This is most likely caused by internal motion within the spacecraft affecting the interferometer. The glitch can be somewhat compensated for by averaging many icks from the same ock, but this isn't recommended for most applications. Bolometer/albedo data is not affected by the glitch. |
Revision as of 16:14, 1 November 2013
Contents: Description, Procedure, Functions Used, Related Functions
Description <<<<UNDER CONSTRUCTION>>>> This procedure illustrates the method to deconvolve TES spectra.
Procedure (1) Find TES Spectra in JMARS
A note on JMARS atmospheric-adjusted emissivity spectra: These spectra are derived by deconvolving the spectra using a standard set of surface and atmosphere endmembers. This works well for a first pass, but may remove surface features since many mineral endmembers are not in this standard library. So, while you could use this data set for more detailed work, it is highly recommend to redo the atmosphere removal with your full mineral library.
hga_motion = 1 (min) to 1 (max). pnl_motion = 1 (min) to 2 (max).
ock (min) = 1583.
ock (max) = 7000. For ocks above 7000, the TES detectors sometimes exhibit an instrumental error (the "glitch") that results in a reversal of the dust absorption near 1100 wavenumbers, creating a broad peak with random direction (peak or trough) and amplitude in the spectra centered around 1000 wn, and extending between 900-1100 wn. This is most likely caused by internal motion within the spacecraft affecting the interferometer. The glitch can be somewhat compensated for by averaging many icks from the same ock, but this isn't recommended for most applications. Bolometer/albedo data is not affected by the glitch.
tot_ice = (min) 0.00 (max) 0.04 tot_dust = (min) 0.00 (max) 0.15
(2) Download emissivity spectra
(3) Load spectra and spectral library into Davinci
dv> tes = split_ock("file.txt")
dv> pplot(tes.ock6002avgcat,xaxis = lib.xaxis,x1 = 1300,x2 = 200)
dv> lib = load("speclib.hdf")
dv> atm = load("atm.hdf")
(4) Remove atmospheric component
dv> endmember 43 is surface dust, remove for atm correction dv> pplot((unmix1.rematm,unmix1.modsur),xaxis = lib.xaxis,x1 = 1300,x = 200
(5) Deconvolve surface spectrum dv> unmix2 = sma(unmix1.rematm,lib,wave1 = 232,wave2 = 1302,nn = 1,exclude = 43) dv> summary_sma(unmix2,1,1,group = 1)
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