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Titel |
Improved instrumental line shape monitoring for the ground-based, high-resolution FTIR spectrometers of the Network for the Detection of Atmospheric Composition Change |
VerfasserIn |
F. Hase |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1867-1381
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Digitales Dokument |
URL |
Erschienen |
In: Atmospheric Measurement Techniques ; 5, no. 3 ; Nr. 5, no. 3 (2012-03-23), S.603-610 |
Datensatznummer |
250002633
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Publikation (Nr.) |
copernicus.org/amt-5-603-2012.pdf |
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Zusammenfassung |
We propose an improved monitoring scheme for the instrumental line shape
(ILS) of high-resolution, ground-based FTIR (Fourier Transform InfraRed)
spectrometers used for chemical monitoring of the atmosphere by the Network
for Detection of Atmospheric Composition Change (NDACC). Good ILS knowledge
is required for the analysis of the recorded mid-infrared spectra. The new
method applies a sequence of measurements using different gas cells instead
of a single calibration cell. Three cells are used: cell C1 is a refillable
cell offering 200 mm path length and equipped with a pressure gauge (filled
with 100 Pa N2O), cells C2 and C3 are sealed cells offering 75 mm path
length. C2 is filled with 5 Pa of pure N2O. Cell C3 is filled with 16
Pa N2O in 200 hPa technical air, so provides pressure-broadened
N2O lines. We demonstrate that an ILS retrieval using C1 improves
significantly the sensitivity of the ILS retrieval over the current
calibration cells used in the network, because this cell provides narrow
fully saturated N2O lines. The N2O columns derived from C2 and C3
allow the performance of a highly valuable closure experiment: adopting the
ILS retrieved from C1, the N2O columns of C2 and C3 are derived.
Because N2O is an inert gas, both columns should be constant on long
timescales. Apparent changes in the columns would immediately attract
attention and indicate either inconsistent ILS results or instrumental
problems of other origin. Two different cells are applied for the closure
experiment, because the NDACC spectrometers observe both stratospheric and
tropospheric gases: C2 mimics signatures of stratospheric gases, whereas C3
mimics signatures of tropospheric gases. |
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