Monitoring Turbulence Height with a DIMM |
ATACAMA WORKSHOP, Ithaca NYM. Sarazin, June 15-17 2000, 9/14 |
The atmospheric seeing (black lower curve, in arcsec) is the cumulative effect of several turbulent layers at various altitudes: monitoring the characteristic altitude of the turbulence (red upper curve, in km) is necessary for planning adaptive optics instrumentation. In this example, the bad seeing is located at low altitude while good conditions are produced by a few layers at high altitude. |