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Link: European Southern Observatory (c) ESO

ESO in-kind Projekt

Universität Innsbruck

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  • In-Kind Projects - Innsbruck

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    • SKY MODEL ONLINE

    • Projects which had final review Thursday March 22, 2012:
    • DR05:
      A new sky model for exposure time calculators (ETCs)
    • DR06:
      Fitting routines for spectra: determination of PWV, molecular abundances and telluric feature correction
    • DR07:
      An advanced sky correction tool for the optical to the NIR.

    • Projects started in 2012:
    • SM01:
      Advanced Sky Model
    • SM02:
      Estimating Atmospheric Parameters
    • SM03:
      Correcting for the Sky Signature

    • Intranet of the Project


Finanziert durch:
BM:wfw

Project DR05 is dedicated to the development of a new sky background model for present and future
ESO-Exposure Time Calculators (ETCs).

The Code is segmented to two individual modules. Module 1 only runs once if the theoretical input data chages. It creates a whole library of template spectra. The whole runtime is a few CPU hours. Module 2 is that part running each time (as a plug-in to the instrument specific ETCs) an observer queries an ETC. It calculates on the fly fast changing (but not CPU intensive) contributions like moon illumination, telescope emission etc. FOr the radiative transfer part it accesses the library data base and interpolates in the given parameter space.

Module 1 creates a synthetic sky spectra library based on data  from HITRAN and meteorological statistical information of the ESO sites. The HITRAN 2008 database (Version 13.0) gives spectral lines of up to 39 molecules and atoms. The meteorological data is taken from the Paranal Meteo-Monitor and is used
to define a parameter space grid for average weather conditions of the observing site Paranal. For each data
point of this grid an atmospheric profile is calculated by merging an atmospheric standard profile and the GDAS profiles (see examples for profiles [Figure]) provided online by NOAA . Both, the atmospheric profiles and the HITRAN spectrum are used as input for the third party radiative transfer code packages LBLRTM and RFM, which create a synthetic sky spectrum for each of the corresponding atmospheric profiles. There are some differences in irradiance [Figure] and in transmission [Figure] between the results of the codes. This is due to different levels of complexity in implimented physics processes. As Module 1 is intended to create a synthetic sky spectra library, which is subsequently used as input for Module 2, it has to be run only once for each newly created HITRAN input.

Module 2 of the DR05 project aims at adding the background model components, which require only small amounts of computing time. Hence, these routines can be carried out during every single ETC call. These components are the scattered Moon and zodiacal light, the telescope emission, and the non-thermal atmospheric continuum and emission lines. All components are added to the spectrum selected from the library, which is best correlated to the user input selections. Module 2 is linked to Module 1 by re-using the molecular radiance and transmission spectra produced by the first component. The maximum wavelength range and resolution of the Module 2 output spectra depend on the corresponding values for the Module 1 library data. Wavelengths between 0.3 and 30 μm and a resolution of 3 − 4 × 105 are guaranteed.

Here an example for the final model [Figure] is shown.

The whole user documentation is given in the ESO document archive as Nr.: VLT-MAN-ESO-19550-5205

The SM01 project mostly already overcomes the DR05 project description - In particular, the model described in Noll et al. (2012) is fully implemented - find it as draft HERE.

Preliminary interface to a calculator extending parameter space compared to the pure ETC is provided also ONLINE. Please cite / reference the scientific use and iform the team about such success stories.

dr05_module1 dr05_module2
Module 1: This module creates a library of synthetic sky spectra on the basis of the HITRAN 2008 database and an atmospheric profile. Module 2 calculates the components, which need only minimal computing time. Hence, these components are computed during every ETC call. The final sky background spectrum is obtained by merging the appropriate synthetic sky spectrum fromModule 1 (selected by user defined input) with these "fast" components.



© 2011-2014 Stefan Kimeswenger - Institute for Astro- and Particle Physics Innsbruck, Austria