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Measurements of the NO2 absorption cross-section from 42 000 cm−1 to 10 000 cm−1 (238–1000 nm) at 220 K and 294 K

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TLDR
In this article, the authors measured the NO2 absorption cross-section from 42 000 to 10 000 cm−1 (238-1000 nm) with a Fourier transform spectrometer (at the resolution of 2 cm− 1, 0.01 nm at 240 nm to 0.2 nm at 1000 nm).
Abstract
The NO2 absorption cross-section has been measured from 42 000 to 10 000 cm−1 (238–1000 nm) with a Fourier transform spectrometer (at the resolution of 2 cm−1, 0.01 nm at 240 nm to 0.2 nm at 1000 nm) and a 5 m temperature controlled multiple reflection cell. The uncertainty on the cross-section is estimated to be less than 3% below 40 000 cm−1 (λ > 250 nm) at 294 K, 3% below 30 000 cm−1 (λ > 333 nm) at 220 K, but reaches 10% for higher wavenumbers. Temperature and pressure effects have been observed. Comparison with data from the literature generally shows a good agreement for wavenumbers between 37 500 and 20 000 cm−1 (267–500 nm). Outside these limits, the difference can reach several percent.

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The HITRAN molecular spectroscopic database: edition of 2000 including updates through 2001

TL;DR: The HITRAN compilation consists of several components useful for radiative transfer calculation codes: high-resolution spectroscopic parameters of molecules in the gas phase, absorption cross-sections for molecules with very dense spectral features, aerosol refractive indices, ultraviolet line-by-line parameters and absorptionCross-sections, and associated database management software.
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Measurements of molecular absorption spectra with the SCIAMACHY pre-flight model: instrument characterization and reference data for atmospheric remote-sensing in the 230–2380 nm region

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TL;DR: In this paper, an algorithm for the near-real time retrieval of tropospheric NO2 columns from the Ozone Monitoring Instrument (OMI) is presented. But the method is based on the combined retrieval-assimilation-modeling approach developed at KNMI for off-line NO2 from the GOME and SCIAMACHY satellite instruments.
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References
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Journal ArticleDOI

The influence of nitrogen oxides on the atmospheric ozone content

TL;DR: In this paper, the probable importance of NO and NO2 in controlling the ozone concentrations and production rates in the stratosphere is pointed out and some processes which may lead to production of nitric acid are discussed.
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On the interpretation of zenith sky absorption measurements

TL;DR: In this article, it is shown that the conversion of NO to NO2 can be of significance in the interpretation of measurements made near twilight and that multiple scattering from the atmosphere or by clouds is likely to be a very small effect.
Journal ArticleDOI

Direct measurements of atmospheric CH2O, HNO2, O3, NO2, and SO2 by differential optical absorption in the near UV

TL;DR: In this paper, measurements of CH2O, HNO2, O3, NO2, and SO2 at four different sites in western Europe are reported, and the mixing ratios of the pollution indicators SO2 and NO2 are < 0.5-2 ppb.
Journal ArticleDOI

Temperature dependent NO2 cross sections at high spectral resolution

TL;DR: In this paper, the authors presented cross sections of NO2 in the spectral region 350-585 nm at four temperatures between 217 and 298 K and total pressures between 100 and 600 torr at a mixing ratio of 84.1 ppmv and at a spectral resolution sufficient for accurate convolution with instruments typically used to measure atmospheric NO2.
Journal ArticleDOI

Photochemistry of NOx and HNOx Compounds

TL;DR: In this article, cross sections for absorption of radiation between 190 and 700 nm were given for N2O, NO2, NO3, NO4, NO5, HNO2, and HNO3.
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