An atmospheric radiation model for Cerro Paranal - I. The optical spectral range

By Stefan Noll, W. Kausch, M. Barden, A. Jones, C. Szyszka, Stefan Kimeswenger, J. Vinther. 2012

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Aims. The Earth’s atmosphere affects ground-based astronomical observations. Scattering , absorption, and radiation processes deteriorate the signal-to-noise ratio of the data received. For scheduling astronomical observations it is, therefore, im portant to accurately estimate the wavelength-dependent effect of the Earth’s atmosphere on the observed flux. Methods. In order to increase the accuracy of the exposure time calcul ator of the European Southern Observatory’s (ESO) Very Larg e Telescope (VLT) at Cerro Paranal, an atmospheric model was developed as part of the Austrian ESO In-Kind contribution. It includes all relevant components, such as scattered moonlight, scat tered starlight, zodiacal light, atmospheric thermal radi ation and absorption, and non-thermal airglow emission. This paper focuses on atmospheric scattering processes that mostly affect the blue ( 0.55� m) wavelength regime. While the former is mainly investigated by means of radiative transfe r models, the intensity and variability of the latter is stud ied with a sample of 1186 VLT FORS 1 spectra. Results. For a set of parameters such as the object altitude angle, Moon-object angular distance, ecliptic latitude, bimonthly p eriod, and solar radio flux, our model predicts atmospheric radiati on and transmission at a requested resolution. A comparison of our model with the FORS 1 spectra and photometric data for the night-sky brightness from the literature, suggest a model accuracy o f about 20%. This is a significant improvement with respect to existing pr edictive atmospheric models for astronomical exposure time calculators.

Subfields: Atmospheric Science, Global and Planetary Change, Spectroscopy

View Paper: https://www.semanticscholar.org/paper/51e735fde0fc4b587e5d6cf42a93831a04dabaff

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