1 / 21

Astrophysics from Space Lecture 2: Beating the atmosphere

Astrophysics from Space Lecture 2: Beating the atmosphere. Prof. Dr. M. Baes (UGent) Prof. Dr. C. Waelkens (KUL) Academic year 2013-2014. The Earth atmosphere. Lord Rayleigh (1842-1919). The Earth atmosphere.

fawn
Download Presentation

Astrophysics from Space Lecture 2: Beating the atmosphere

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Astrophysics from Space Lecture 2: Beating the atmosphere Prof. Dr. M. Baes (UGent) Prof. Dr. C. Waelkens (KUL) Academic year 2013-2014

  2. The Earth atmosphere Lord Rayleigh (1842-1919)

  3. The Earth atmosphere Relative concentrations of permanent gases in the atmosphere is relatively constant. Non-permanent gases: H20 and O3

  4. Water vapor in the atmosphere H20 (and CO2 to some extent) are responsible for most of the extinction in the optical and NIR regime Good news: H20 is low-altitude phenomenon

  5. Mauna Kea – Hawaii

  6. La Silla – Chile

  7. Paranal – Chile

  8. Optical observatories Most large ground-based optical/NIR observatories are located on mountain tops

  9. Diffraction of light Diffraction is a natural consequence of the wave nature of light. Airy diffraction pattern

  10. Diffraction of light Airy diffraction: point sources are converted to a disc (Airy disc) with size θmin ~ 1.22 λ/D Example: VLT with D = 8.2 m optical radiation at λ = 550 nm θmin = 0.014 arcsec Unfortunately, it is currently impossible to realize diffraction limited observations in the optical, due to optical aberrations in the telescope and atmospheric turbulence.

  11. Active optics Elimination of the aberrations in the telescope optics by (continuous) correction of the telescope shape. Result: seeing-limited observations

  12. Atmospheric turbulence Atmospheric turbulence spreads out optical radiation to a much bigger disk (seeing disc) than the diffraction limit.The seeing depends critically on the site. Typical seeing values: Belgium: few arcsecLa Palma: 1 arcsec Paranal: 0.6 arcsec Dome C: 0.3 arcsec

  13. Atmospheric turbulence = In seeing-limited observing, the 8 m VLT telescope has the same resolution as an amateur 30 cm telescope

  14. Beating the atmosphere Seeing is the result of “speckles” moving on the plane of the sky at atmospheric time scales 10 ms to 100 ms

  15. Speckle imaging and Lucky imaging Use very fast, short-exposure images and combine them at the end of the observation - Speckle imaging: combine all images - Lucky imaging: select only the “best” images Traditional image Exposure time 300s Speckle imageExposure time 300s Lucky image Exposure time 15s

  16. More Lucky imaging examples Cat’s Eye nebula Globular cluster M13

  17. Adaptive optics 1. Measure the distortions in the wavefront 2. Compensate for them using deformable mirror or liquid crystal array

  18. Adaptive optics Advantage of AO: one can keep integrating(so not limited to bright sources as speckle/Lucky imaging) Problem: bright reference star necessary: NGS/LGS

  19. Adaptive optics

  20. Adaptive optics Still many problems - Reliable LGS AO systems are still rare… - Atmospheric conditions must be optimal for AO - Turbulence cells are typically smaller than telescope -> multi-conjugate AO

  21. The solution: space telescopes

More Related