A robotic instrument for measuring high altitude atmospheric turbulence from Dome C, Antarctica

To properly characterize the atmospheric properties of a site for a future large telescope or interferometer, it is insufficient to measure quantities, such as the full-width at half-maximum of a stellar image, that have been integrated over the entire atmosphere. A knowledge of the turbulence distr...

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Bibliographic Details
Main Authors: Lawrence, J. S., Ashley, M. C. B., Kenyon, S., Storey, J. W. V., Tokovinin, A., Lloyd, J. P., Swain, M.
Other Authors: Oschmann, Jacobus M.
Format: Book Part
Language:English
Published: Society of Photo-optical Instrumentation Engineers (SPIE) 2004
Subjects:
Online Access:https://authors.library.caltech.edu/92278/
https://authors.library.caltech.edu/92278/1/174.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20190115-103112848
Description
Summary:To properly characterize the atmospheric properties of a site for a future large telescope or interferometer, it is insufficient to measure quantities, such as the full-width at half-maximum of a stellar image, that have been integrated over the entire atmosphere. A knowledge of the turbulence distribution as a function of height is necessary, since this affects the ease and degree to which adaptive optics systems can improve the telescope’s resolution. Furthermore, some astronomical measurements, such as narrow-field differential astrometry at microarcsecond precision, depend critically on the amount of turbulence high in the atmosphere (up to 20km). In order to obtain the necessary site-testing data at remote sites such as those on the Antarctic plateau, we have designed a robust and reliable instrument based on an 85 mm refractive telescope, a gimbal-mounted sidereostat mirror, and a Multi-Aperture Scintillation Sensor (MASS). The instrument uses the spatial structure of single-star scintillation to measure vertical turbulence profiles from 0.5 to 20km. The MASS system is designed to operate completely autonomously throughout the Antarctic winter. It also has potential applications at existing observatory sites for quantifying the turbulence characteristics of the atmosphere in real-time.