High spectral resolution ozone absorption cross-sections - Part 2: Temperature dependence
By A. Serdyuchenko, V. Gorshelev, Mark Weber, W. Chehade, John P. Burrows. 2013
452 citations recorded by the source corpus.
Abstract. We report on the temperature dependence of ozone absorption cross-sections measured in our laboratory in the broad spectral range 213–1100 nm with a spectral resolution of 0.02–0.24 nm (full width at half maximum, FWHM) in the atmospherically relevant temperature range from 193 K to 293 K. The temperature dependence of ozone absorption cross-sections was established using measurements at eleven temperatures. This investigation is superior in terms of spectral range and number of considered temperatures compared to the previous studies. The methodology of the absolute broadband measurements, experimental procedures and spectra processing were described in our companion paper together with the associated uncertainty budget. In this paper, we report in detail on our data below room temperature and compare them with literature data using direct comparisons as well as the standard approach using a quadratic polynomial in temperature fitted to the cross-section data.
Subfields: Atmospheric Science, Global and Planetary Change, Spectroscopy
View Paper: https://www.semanticscholar.org/paper/134274e7d0ce0b2eec6ad946b1e6adec14dc896c
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In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Planetary Spectrum Generator: An accurate online radiative transfer suite for atmospheres, comets, small bodies and exoplanets (2018, background): “The MPI-Mainz UV/VIS Spectral Atlas [34] UV cross-sections for O3 [35] UV cross-sections for CO2 [36] Wavelength range: 0.”
- Comparison of TROPOMI/Sentinel-5 Precursor NO2 observations with ground-based measurements in Helsinki (2019, unknown): “…correction to the cross-sections used in the spectral fitting procedure based on modelled monthly average NO 2 and temperature profiles and high-resolution temperature-dependent cross sections by Vandaele et al. (1998) for NO 2 and Serdyuchenko et al. (2014) for O 3 (as in the TROPOMI retrieval).”