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Validation of millimetre and sub-millimetre atmospheric collision-induced absorption at Chajnantor

Due to the importance of a reference atmospheric radiative transfer model for both planning and calibrating ground-based observations at millimetre and sub-millimetre wavelengths, we have undertaken a validation campaign consisting of acquiring atmospheric spectra under different weather conditions,...

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Bibliographic Details
Published in:Astronomy and astrophysics (Berlin) 2025-01, Vol.693, p.A148
Main Authors: Pardo, J. R., De Breuck, C., Muders, D., González, J., Pérez-Beaupuits, J. P., Cernicharo, J., Prigent, C., Serabyn, E., Montenegro-Montes, F. M., Mroczkowski, T., Phillips, N., Villard, E.
Format: Article
Language:English
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Summary:Due to the importance of a reference atmospheric radiative transfer model for both planning and calibrating ground-based observations at millimetre and sub-millimetre wavelengths, we have undertaken a validation campaign consisting of acquiring atmospheric spectra under different weather conditions, in different diurnal moments and seasons, with the Atacama Pathfinder EXperiment (APEX), due to the excellent stability of its receivers and the very high frequency resolution of its back-ends. As a result, a dataset consisting of 56 spectra within the 157.3–742.1 GHz frequency range, at kilohertz resolution (smoothed to ∼2–10 MHz for analysis), and spanning one order of magnitude (∼0.35–3.5 mm) in precipitable water vapour columns, has been gathered from October 2020 to September 2022. These data are unique for their quality and completeness and, due to the proximity of APEX to the Atacama Large Millimeter/Submillimeter Array (ALMA), they provide an excellent opportunity to validate the atmospheric radiative transfer model currently installed in the ALMA software. The main issues addressed in the study are possible missing lines in the model, line shapes, vertical profiles of atmospheric physical parameters and molecular abundances, seasonal and diurnal variations, and collision-induced absorption (CIA), to which this paper is devoted, in its N 2 –N 2 + N 2 –O 2 + O 2 –O 2 (dry) and N 2 –H 2 O + O 2 –H 2 O (‘foreign’ wet) mechanisms. All these CIA terms should remain unchanged in the above-mentioned ALMA atmospheric model as a result of this work.
ISSN:0004-6361
1432-0746
DOI:10.1051/0004-6361/202452159