Paper
4 August 2010 Measuring the water vapor above the SOFIA Observatory
Author Affiliations +
Abstract
The SOFIA airborne observatory flies in the lower stratosphere above more than 99.9% of the Earth's water vapor. As low as this residual water vapor is, it will still affect SOFIA's infrared and sub-millimeter astronomical observations. As a result, a heterodyne instrument operating at 183 GHz will be used to measure the integrated water vapor overburden in flight. The accuracy of the measured precipitable water vapor must be 2 microns or better, 3 sigma, and measured at least once a minute. This presentation will cover the design and the measured laboratory performance of this instrument, and will discuss other options for determining the water vapor overburden during the SOFIA Early Science shared-risk period.
© (2010) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Thomas L. Roellig, Lunming Yuen, David Sisson, and Allan Meyer "Measuring the water vapor above the SOFIA Observatory", Proc. SPIE 7733, Ground-based and Airborne Telescopes III, 773339 (4 August 2010); https://doi.org/10.1117/12.856506
Lens.org Logo
CITATIONS
Cited by 1 scholarly publication.
Advertisement
Advertisement
RIGHTS & PERMISSIONS
Get copyright permission  Get copyright permission on Copyright Marketplace
KEYWORDS
Atmospheric modeling

Radiometry

Observatories

Control systems

Infrared astronomy

Astronomy

Infrared radiation

RELATED CONTENT

An overview of the planned CCAT software system
Proceedings of SPIE (July 18 2014)
Site conditions for astronomy at the South Pole
Proceedings of SPIE (August 21 1998)
German Center for Interferometry FrInGe
Proceedings of SPIE (February 21 2003)

Back to Top