Astrophysics (Index)About

seeing

(apparent blurring and twinkling of objects seen through atmosphere)

Astronomical seeing is the blurring of objects seen through the atmosphere. When using a ground-based telescope, even a long exposure will result in point and line details being turned into finite blobs and "bars", due to continuous changes in the optical characteristics of the atmosphere.

A seeing limited telescope's angular resolution limit is ultimately due to this phenomena. In contrast, a telescope in space or a ground-based telescope that can cancel these effects is limited by diffraction and is termed diffraction limited. Atmospheric effects are caused by density variations in the atmosphere over time and space. These effects can be reduced by locating telescopes at high altitude, by favorable weather conditions, by large telescopes, and by adaptive optics. The effects vary over time, some nights being better than others (i.e., calm nights), and the seeing may change by the minute.

A seeing number is a measure of seeing, an expression of how far from "true" a point might appear on the focal plane, or as observations often take time, and the atmospheric effects change continuously, how big the spot is on the focal plane from the point (e.g., a distant star) due to the atmospheric turbulence. Since the aperture of the telescope already limits its resolution by turning the point into an Airy disk, the seeing number may be added to that angular resolution to give some hint as to the resulting resolution of an observation. The seeing number is typically the full width at half maximum (FWHM), i.e., given an exposure time much longer than the changes in seeing due to turbulence, the point will be seen at different points in time around a circle in the focal plane, mostly in the center, and the further from that center, the less often. The FWHM seeing number is half the diameter of the circle that includes the most extreme distortion, and is expressed in arcseconds, as is a telescope/instrument's resolution due to Airy disks.

Other measures are r0 (Fried parameter) and t0 (Greenwood time constant). The former is an aperture size sufficiently small that seeing distortions would be minor, and the latter is a time interval estimating how long an exposure could be before seeing distortions are likely to be significant. Aside from specifying seeing for telescope observers, they are basic parameters in the design of AO systems.


(telescopes,optics,atmosphere,turbulence)
Further reading:
http://en.wikipedia.org/wiki/Astronomical_seeing
https://www.innovationsforesight.com/education/astronomical-seeing-tutorial/
https://content.meteoblue.com/nl/spatial-dimensions/air/astronomy-seeing
http://www.ifa.hawaii.edu/~meech/a281/handouts/seeing.pdf

Referenced by pages:
aerosols
atmosphere
diffraction limited
guide star (GS)
imaging Fourier transform spectroscopy (IFTS)
Infrared Telescope Maffei (ITM)
Malmquist bias
Roque de los Muchachos Observatory (ORM)
pointing error (PE)
plate scale
shift-and-add
speckle imaging
speckle masking
telescope
tomography
turbulence
twinkling
wavefront error (WFE)

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