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Widefield Imaging at Long Wavelengths

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Wide-field Imaging at Long Wavelengths. Joseph Lazio ... Limits to wide-field imaging at long-wavelengths being reached with current arrays. ... – PowerPoint PPT presentation

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Title: Widefield Imaging at Long Wavelengths


1
Wide-field Imaging at Long Wavelengths
  • Joseph Lazio
  • Namir Kassim, Aaron Cohen, Wendy Lane (Naval
    Research Laboratory)

2
Scientific Motivations
  • VLA, GMRT, LWA, LOFAR,
  • Surveys for high-z AGN
  • Searches for radio halos and relics
  • Acceleration processes
  • Are clusters relaxed?
  • Dark energy?
  • Extrasolar planets
  • Transients?
  • e.g., GCRT J1745-3009
  • SKA Key Science Projects
  • Galaxy Evolution, Cosmology, and Dark Energy
  • Galaxy power spectrum
  • Weak lensing
  • Probing the Dark Ages
  • Finding the first AGN
  • H I absorption toward AGN during the Epoch of
    Reionization
  • The Origin of Cosmic Magnetism?

Often it is not that the source of interest is
large, but that the field of view is large and
filled with nuisance sources.
3
Long Wavelength Array (LWA)
  • Returning to roots of radio astronomy
  • Several technological issues solved from
    previous generation of instruments
  • Frequency range 2080 MHz
  • Initial operation in 2008
  • Southwest Consortium (NRL, UNM, UTARL, LANL)
  • http//lwa.nrl.navy.mil/

4
Wide-Field Imaging Requirements
  • 74 MHz VLA
  • 11º field of view
  • 10 km baselines (B config.)
  • 35 km baselines (A config.)
  • 70 km baselines (VLAPT)
  • LWA
  • 3º5 º field of view over 2080 MHz
  • 400 km baselines
  • SKA
  • 50100 deg.2 field of view near 500 MHz
  • lt 150 km baselines?
  • goal is for SKA to operate down to 60 MHz(!)

74 MHz VLA field of view 11º
5
Current Wide-field Imaging
  • Self-calibration
  • Strong sources
  • Field-based calibration (Cotton Condon 2002)
  • Limited baselines ( 10 km)
  • VLA Low Frequency Sky Survey (VLSS)
  • w-projection ?

6
Self-calibration
(T. Delaney, L. Rudnick)
7
Self-calibration II
  • VLAPT Cgynus A
  • 10 resolution
  • still not high enough resolution
  • like to be able to do more than just the
    brightest sources in the sky

8
ChallengeIonospheric Remediation
Wedge Effects Faraday rotation, refraction Wave
Effects Rapid phase fluctuations These are the
easy parts!
50 km
Wedge characterized by TEC ?nedl
1017 m-2 Introduces extra electrical
path length ?L ? ?2 ? TEC Adds extra
phase ?? ?L?? ? Waves tiny (lt1)
fluctuations superimposed on the wedge
Wedge
VLA
  • The wedge introduces thousands of turns of
    electrical phase at 74 MHz.
  • A long wavelength interferometer is extremely
    sensitive to differences in phase and sees the
    much smaller superimposed waves very clearly
    even if it samples only a fraction of a wave.

We routinely derive DTEC maps of structures as
small as 100 m, varying on timescales shorter
than a minute, spread over a field of 10o, with
sub-milliTECU precision.
9
Exquisite Sensitivity to Fine-Scale Ionospheric
Phenomena
  • Phase variation on three 8-km VLA spacings at 3
    different azimuths
  • Wide range of ionospheric phenomena seen
  • Some of the ionospheric phase fluctuations arise
    from the sporadic E-layer in the ionosphere?

(Perley)
10
ChallengeIonospheric Remediation II
  • Self-calibration useful for correcting in a given
    direction (or over a small field).
  • Field of view of antennas sees a large, and
    different, portion of the ionosphere.

(antennas, not stations)
11
Differential Ionospheric Refraction
  • These nine radio sources were selected from a
    deep 74 MHz image.
  • The individual 30-second maps were compiled as
    animations of the nine hour measurement, running
    from nighttime through two hours past sunrise.
  • The variations in position, peak intensity, and
    sidelobe structure show the effects of
    differential ionospheric refraction across the
    field.

12
Field-based Calibration
  • Take snapshot images of bright sources in the
    field and compare to known positions.
  • Fit to a 2nd order Zernike polynomial phase
    delay screen for each time interval.
  • Apply time variable phase delay screen to
    produce corrected image.

Self-Calibration
Field-Based Calibration
13
Limits to Correction Method
Image Distortion
12 km Isoplanatic Patch (best we can do)
35 km Isoplanatic Patch
Sidelobe Confusion
15?
Striping due to sidelobe confusion from a far-off
source in a completely different IP
14
Facetted Imaging
  • 12 km baselines (B configuration) of 74 MHz VLA
  • 300 facets
  • 36 km baselines (A configuration) of 74 MHz VLA
    requires 10x more
  • 3000 facets
  • 108 pixels
  • gt 100 km baselines of LWA means another order of
    magnitude

15
Future?w-projection
  • Project the 3-dimensional visibilities to the (u,
    v) plane.
  • Suggested originally by Frater Doherty (1980)
  • Implemented by Cornwell, Golap, Ghatnagar
    (2004).
  • V(u, v, w) G(u, v, w) V(u, v, 0)
  • Fresnel diffraction of radiation field from one
    antenna to another
  • Convolutions inexpensive to implement with large
    memory systems.

Per A
16
Long Wavelength Imaging
17
Summary
  • Limits to wide-field imaging at long-wavelengths
    being reached with current arrays.
  • SKA, LWA, etc. will be even more challenging.
  • Existing methods do have regimes of
    applicability.
  • Self-calibration for strong sources.
  • Field-based calibration for intermediate
    baselines.
  • Future
  • W-projection is a clear improvement for
    wide-field imaging.
  • What about ionosphere?
  • Basic research in radio astronomy at the NRL is
    supported by the Office of Naval Research.

18
FINITO
19
Long Wavelength Imaging
20
Extending resolution and uv coverage Impact of
outlying elements
VLA alone
Spatial Frequency
21
LWA Opening a New Window on the Universe
Current Capabilities
Proposed LWA
22
Addressing Ionospheric Issue
  • More aggressive empirical approaches
  • Develop more robust, high-order corrections based
    on optical approaches.
  • Woods and Greenaway method tested by NPOI group,
    enables use of Zernike components to order gt 80
    accounts for nonuniform distributions, variable
    intensities.
  • Develop Kalman propagator to impose physicality
    on time variation.
  • Physical model-based corrections
  • Can we ingest empirical correction data, or even
    raw data into physical models within GAIM or
    IDA, and then use those models to provide better
    conditioned corrections?
  • Opportunity to get improved understanding of
    ionospheric phenomenology to which we are
    uniquely sensitive.
  • E.G., VLA data coupled with airglow imagery may
    distinguish phenomena occurring in E and F
    layers.

23
Challenge Wide-Field Imaging
  • NRL NRAO were the first to implement practical
    solutions to wide-field imaging with non-coplanar
    arrays.
  • Problem Current approaches insufficient for
    future instruments.
  • Approximation of 3D inversion with tessellated 2D
    facets is computationally unfeasible with much
    larger arrays.
  • Even current VLA facet-based method introduces
    errors.
  • New w-projection technique under development.
  • Projection of intrinsically 3-D data to 2-D
    plane, with an appropriate Fresnel-like
    convolution.
  • Suggested in the early 1980s, computational power
    just now becoming capable of implementing it.
  • Removes reliance on tessellation generates one
    contiguous distortion-free image.
  • Order of magnitude faster than facet-based
    methods.
  • We think this will work for the emerging large
    arrays.
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