Lecture 4: Atmospheric Turbulence Flashcards

(64 cards)

1
Q

layers of the atmosphere

A

earth
troposphere
stratosphere
mesosphere
ionosphere

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2
Q

at 50km, pressure has fallen to around 1 mbar so

A

little turbulence above this altitude

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3
Q

temperature variations giving rise to optical effects of turbulence only significant in

A

the troposhere

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4
Q

where is turbulence usually greatest

A

nearest the ground

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5
Q

turbulence falls of exponentially with increasing altitude except

A

for peak that occurs at the tropopause

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6
Q

Peak that occurs at the tropopause is due to

A

wind shear

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7
Q

wind shear gives rise to

A

kelvin-helmholtz instabilities

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8
Q

kolmogorov model - energy added to fluid in the form of

A

large scale disturbances

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9
Q

kolmogorov model - eddies or vortices generated on

A

outer scale
L0

spawns cascade on smaller eddies

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10
Q

kolmogorov model - turbulence dies away at

A

inner scale
l0

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11
Q

kolmogorov model - kinetic energy dissipated by

A

viscosity

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12
Q

kolmogorov model - outer scale L0 is typically

A

10m

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13
Q

kolmogorov model - inner scale l0 is typically

A

few mm

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14
Q

kolmogorov model - stable state…

A

rate of input of turbulent energy =
rate of viscous dissipation

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15
Q

kolmogorov model - fluctuations in velocity are governed only by

A

scale, l , and the rate of energy input/dissipation per unit mass, epsilon

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16
Q

kolmogorov model - epsilon

A

rate of energy per unit mass

(units of J/s/kg)

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17
Q

kolmogorov model - scale

A

l
units m

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18
Q

structure functions were introduced by Kolmogorv to describe

A

non-stationary random functions encountered in turbulence

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19
Q

structure functions - temporal - use

A

difference function
F(τ)=f(t+τ)-f(t)

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20
Q

structure function

A

average of square difference

F(τ)= <[T(τ)]^2> = <[f(t+τ)-f(t)]^2>

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21
Q

spatial difference and structure functions

A

same as temporal but replace t with x and τ with r

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22
Q

Structure function of velocity at locations separated by
distance r along a coordinate x

A

D(r)=<[V(x+r)-V(x)]^2> = C_v^2 r^2/3

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23
Q

C_v^2

A

structure parameter for velocity

characterises mechanical turbulence

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24
Q

temperature varies with

A

altitude

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25
mechanical turbulence mixes air at
the tropopause
26
temperature cells
cells or pockets of air with different temperatures
27
Structure function of temperature has same spatial dependence as
structure function of velocity
28
C_T
structure parameter for temperature variations
29
temperature fluctuations affect the
density of air and therefore change its refractive index
30
optical effects produced by
variations in refractive index
31
31
dependence of refractive index on
temperature and pressure
32
local pressure fluctuations smoothed out at
speed of sound negligible effect compared with temperature fluctuations
33
autocorrelation of pupil
area of overlap / total area
34
wavefront distortions - phase shift
thi(x) = 2pi (Delta (nl) / lambda) =2pi (optical path length/lambda)
35
including the effect of wavefront distortion over the pupil, P(X)=
Ψ(x)=e^iphi(x) over aperture 0 elsewhere (before we were just using Ψ=1 over aperture)
36
bold font indicates that this represents
a generalised 2D spatial coordinate
37
coherence function
optical transfer functions of the atmosphere as a result of turbulence at height h
38
given that phi(x) obeys gaussian statistics and has a mean of zero, we can say
coherence func Bh(r)=e^-1/2 phase structure func
39
steps to derive the phase structure function in terms of the strength of refractive index fluctuations
1. D(r) in terms of B(r), the covariance of phase 2. B(r) in terms of B_N(r,z) 3. D(r) in terms of D_N(r,z) via B_N(r,z) and B_phi(r) 4. D(r) in terms of C_N^2
40
delta h much larger than the scale of fluctuation so can
extend integration to -inf to inf
41
atmospheric transfer function
coherence function or optical transfer function of the atmosphere
42
for observations at an angle from the zenith, the thickness of each layer is
increased by the factor sec(angle from zenith)
43
for large telescopes, image filtering/point spread dominated by
atmospheric effects
44
point spread function of the atmosphere
inverse FT of the atmospheric transfer function
45
image intensity
convolution of geometric image with point spread of the atmosphere
46
phase variation across the wavefront is described by
the phase structure function
46
planar wavefronts from the distant source are distorted by
the turbulent layers of the atmosphere
47
by applying the Kolomogorov model, one can
derive the dependence of structure function on atmospheric parameters, specifically the structure parameter
48
structure parameter characterises the
strength of fluctuations in refractive index
49
knowing the phase structure function, one can
derive the optical transfer function of the atmosphere
50
taking the inverse fourier transform of the optical transfer function, one derives the
point spread function due to the atmosphere
51
the observed image is the convolution of
the point spread function with the geometrical image of the star
52
can rewrite the atmospheric transfer function as
B=exp[-3.44(r/r0)^5/3] ro is the fried parameter
53
fried parameter is an indication of
the strength of the phase fluctuations
54
beta
parameter is an angle in radians and is referred to as the seeing of the atmosphere
55
beta is found by
finding FWHM of |h_atm|^2 gives beta = 0.98 lambda / ro
56
seeing is the equivalent resolution one would get by
viewing through a diffraction limited telescope of diameter ro
57
ro is typically about
10-20cm in the visible region of the spectrum
58
regardless of the diameter of the primary mirror, resolution still
corresponds to that of a telescope with a 10cm aperture
59
Wind Shear leads to turbulence and the generation of
turbulence cells
60
the kolomogorov model describes the
variation of temperature and refractive index over a wide range of scales
61
wavefront distortions occure due to
changes in the optical path length
62