Lecture 5: Adaptive Optics Flashcards
(25 cards)
turbulent cells evolve on longer timescales than
time it takes the wind to move a cells by its own size
turbulent cells move by its own size in time
t0 = t2-t1 = approx ro/V
atmospheric time constant or coherence time
t0=r0/V
good observing site, typical night
V=10m/s
r0=10cm (visible spectrum)
t0=10ms
exposure time short
t<t0
exposure time long
t>t0
adaptive optics must operate on timescales
shorter than t0
isoplanatic angle
approx r0/h
isoplanatic angle is the angle over which
turbulence pattern shifted by distance r0
angular separation at which light from two stars becomes uncorrelated
isoplanatic angle, good observing site, typical night
h=10km
ro=10cm
theta 0 2”arc
theta0 determines
area of sky over which adaptive optics are effective
original wavefront restored by
inserting equal and opposite path length corrections producing corrected image
wavefront compensation - correction carried out in
reflection by deformable mirror
adjusted in shape to match wavefront
adaptive optic scheme
- plane wavefront from star corrugated by turbulence in atmos
- diverging beam beyond telescope made parallel by collimator
- collimated beam reflects off deformable mirror
- unwanted light picked off by dichroic beamsplitter
- focused onto wavefront sensor
wavefront sensor needs bright point source to
provide sufficient signal to noise in a short exposure time
strehl ratio - effect of
wavefront compensation on the intensity profile of a turbulence-degraded image of a star
airy disc - strehl ratio=
1
partial compensation - strehl ratio
<1
no compensation - strehl ratio
«1
compensation of the wavefront transfers energy from
halo of the image (radius lambda/ro) to the core of the image (radius lambda/D)
strehl ratio S=
I_PSF(0)/I_airy(0)
S=(r0/D)^2
the atmospheric seeing is the
resolution resulting from atmospheric turbulence
it is equivalent to the diffraction limited resolution of telescope with diameter r0
the fried paramater is also the
length of the wavefront over which the phase changes by 1 radian
the atmospheric time constant is the
timescale over which a turbulence cells moves by r0