aperture synthesis Flashcards

1
Q

what is aperture synthesis

A

the practical way to make an image with an interferometer

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2
Q

preliminaries for aperture synthesis

A

take an east-west interferometer observing a source at declination delta and hour angle H

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3
Q

hour angle=

A

local siderial time - right ascension

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4
Q

interferometer baseline

A

D=(D,0,0)

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5
Q

path compensation

A

our target is not usually overhead, so we must introduce a physical delay into one arm of the interferometer to compensate

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6
Q

path compensation can be done by

A

switching in physical lengths of real cable or digitally, in memory

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7
Q

as the earth spins, the phase of the correlated signal

A

changes, and we get a fringe rate

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8
Q

what is fringe stopping

A

complex fringe visibility will be rotating at fringe rate in the complex plane and must be constantly rotated backwards to compensate

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9
Q

why do we need to path-compensate?

A

If bandwidth is deltav
⇒ noise signal evolves randomly on timescales of 1/deltav
⇒ must synchronise the two signals (in time) so that the excess path is
≪ c/deltav
This can be done coarsely with path compensation before fine
adjustment with fringe-stopping.

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10
Q

can we use more than two antennas?

A

yes - just take tehm in pairs

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11
Q

n antennas, how many baselines

A

n ways to choose first antenna
(n-1) to choose second
n(n-1) groupings but take away double counting gives
1/2 n(n-1) baseliens

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12
Q

multi-element interferometers are an efficient way to

A

generate many values of complex fringe visibility simultaneously

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13
Q

solution to only getting measurements in one direction

A

space the elements out on the ground in two dimensions

eg the very large array in new mexico:

y-shaped configuration

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14
Q

solution 2 for only getting measurements in one direction

A

let the Earth rotation supply different baseline projected lengths and orientations with respect to the source
“earth rotation aperture synthesis”

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15
Q

what is is that always determines resolution

A

the projection of the baseline perpendicular to the source direction

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16
Q

we should measure Γ(u,v) in what spatial plane

A

plane perpendicular to the source direction:

the (u,v) plane

17
Q

u is parallel to

A

the right ascension direction

18
Q

v is parallel to

A

the declination direction

19
Q

because the sky brightness is real, the fourier transform Γ(u,v) is

A

hermitian conjugate

ie Γ(u,v)= Γ*(-u,-v)

so one half of the (u,v) plane measurements can be deduced form the other half - 12 hours observation needed

20
Q

the synthesised aperture has a synthesised beam defining the

A

angular resolution of the interferometer

21
Q

for an east-west line interferometer, the resolution in declination is

A

poor for low-dec sources

22
Q

advantage of y-shaped interferometer

A

north-south spacings maintain resolution in declination even when dec=0

23
Q

unlike conventional apertures, the synthesised beam of an imaging interferometer can be

A

very ‘dirty; with lots of strong sidelobes

24
Q

if the (u,v)-plane sampling is sparse, we get a

A

heavily degraded (‘dirty’) image, missing many spatial frequencies

25
Q

solution to sparse sampling

A

image reconstruction aka deconvolution

26
Q

image reconstruction

A

an attempt to remove the effects of the convolving beam patttern

27
Q

image reconstruction: the CLEAN algorithm

A

Disassemble the dirty image into many, weak, overlapping versions of the synthesised beam, then reconstruct with cleaner beams (e.g., Gaussians).

28
Q

image reconstruction: the maximum entropy method

A

Determine the ‘least committal’
image consistent with the data. Use the configurational entropy of
any consistent image to quantify its prior probability, and progress
via Bayes Theorem to get the most probable representation of the
source