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The microstructure of the index of refraction and its relationship with "seeing"

Analog statistical properties may be applied to the index of refraction and one may define a structure coefficient of the index of refraction . From equation (gif) and ignoring the very minor effect of humidity, is related to by:

 

where is the wavelength. Normally one considers as a reference the wavelength = 500 nm and the previous equation becomes:

 

The seeing effect through an atmospheric layer of height H can then be expressed an integral function of the index of refraction structure coefficient , whereby the Fried parameter is given by

 

where is the zenithal angle of the direction of observationgif.

Recalling equation (gif), the FWHM spread of the seeing disk in arcsec is then given by:

 

For a vertical direction and = 500 nm, the FWHM angle is expressed as:

  [IMAGE ]
Figure: Parameterisation of seeing FWHM with respect to a mean value of (K m) integrated over a distance z.

Combining with equation (gif), for typical conditions of astronomical mountain sites (pressure 770 mb, temperature 10) one obtains:

 

The diagram at fig. gif illustrates the order of magnitude of the seeing effect with respect to a mean value of and the integration distance. Depending on the geometric scale of the phenomenon causing seeing, the critical values of will be very different: for instance, if we set at 0.1 arcsec an arbitrary threshold for "bad" seeing from a single cause, the corresponding critical (mean) value of will be

Equations (gif) and following show that the overall seeing effects may be considered a 5/3-exponent sum of different terms corresponding to the different atmospheric layers. Thus if is natural seeing FWHM, caused by the boundary layer and upward, and is the local seeing, the overall seeing is:

 

The best astronomical sites are reported to have a natural seeing varying between 0.3 to 0.6 arcsec (FWHM), which is roughly equally divided between the high atmosphere and the atmospheric boundary layer. Acceptable sites for astronomical research will have natural seeing up to 2 arcsec.

Local seeing, that is the seeing caused by the telescope and the surrounding structures can represent anything from zero to about 2 arcsec and can be the cause of very significant differences of image quality among telescopes located on the same site. Fig. gif (page gif) shows the monthly average of seeing values logged at different telescopes located close to one another at the La Silla observatory. The common trends of the plot let observe the seasonal variation of the natural seeing at La Silla, which becomes generally worse during the (austral) winter months. One will also note the large differences among the telescopes and with respect to the DIMM seeing monitor, which are often of the order or 0.5 arcsec and sometimes reach 1 arcsec. Understanding and decreasing these differences, unequivocally caused by the enclosure and the atmospheric environment in the immediate surrounding of the telescope, is the challenge faced by all future telescope projects.



next up previous contents
Next: Effects of wind Up: Thermal turbulencelight Previous: The microstructure of



Lorenzo Zago, lorenzo.zago@heig-vd.ch, Mon Nov 6 23:33:14 GMT+0100 1995