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    Low-Frequency Observations of the Moon with the Murchison Widefield Array

    189880_72902_1538-3881_145_1_23.pdf (1.679Mb)
    Access Status
    Open access
    Authors
    McKinley, B.
    Briggs, Frank
    Kaplan, D.
    Greenhill, L.
    Bernardi, G.
    Bowman, Judd
    de Oliveira-Costa, A.
    Tingay, Steven
    Gaensler, B.
    Oberoi, Divya
    Johnston-Hollitt, M.
    Arcus, Wayne
    Barnes, D.
    Bunton, John
    Cappallo, Roger
    Corey, Brian
    Deshpande, Avinash
    DeSouza, Ludi
    Emrich, D.
    Goeke, Robert
    Hazelton, Bryna
    Herne, David
    Hewitt, Jacqueline
    Kasper, Justin
    Kincaid, Barton
    Koenig, R.
    Kratzenberg, Eric
    Lonsdale, Colin
    McWhirter, S.
    Mitchell, D.
    Morales, Miguel
    Morgan, Edward
    Ord, Stephen
    Pathikulangara, Joseph
    Prabu, T.
    Remillard, Ron
    Rogers, Alan
    Roshi, Anish
    Salah, J.
    Sault, Robert
    Shankar, N Udaya
    Srivani, K.
    Stevens, J.
    Subrahmanyan, R.
    Wayth, R.
    Waterson, Mark
    Webster, Rachel
    Whitney, Alan
    Williams, A.
    Williams, C.
    Wyithe, J.
    Date
    2013
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    McKinley, B and Briggs, Frank and Kaplan, D and Greenhill, L and Bernardi, G and Bowman, Judd and de Oliveira-Costa, A. et al. 2013. Low-Frequency Observations of the Moon with the Murchison Widefield Array. Astronomical Journal 145 (1): 23.
    Source Title
    Astronomical Journal
    DOI
    10.1088/0004-6256/145/1/23
    ISSN
    0004-6256
    URI
    http://hdl.handle.net/20.500.11937/18929
    Collection
    • Curtin Research Publications
    Abstract

    A new generation of low-frequency radio telescopes is seeking to observe the redshifted 21 cm signal from the epoch of reionization (EoR), requiring innovative methods of calibration and imaging to overcome the difficulties of wide-field low-frequency radio interferometry. Precise calibration will be required to separate the expected small EoR signal from the strong foreground emission at the frequencies of interest between 80 and 300 MHz. The Moon may be useful as a calibration source for detection of the EoR signature, as it should have a smooth and predictable thermal spectrum across the frequency band of interest. Initial observations of the Moon with the Murchison Widefield Array 32 tile prototype show that the Moon does exhibit a similar trend to that expected for a cool thermally emitting body in the observed frequency range, but that the spectrum is corrupted by reflected radio emission from Earth. In particular, there is an abrupt increase in the observed flux density of the Moon within the internationally recognized frequency modulated (FM) radio band. The observations have implications for future low-frequency surveys and EoR detection experiments that will need to take this reflected emission from the Moon into account. The results also allow us to estimate the equivalent isotropic power emitted by the Earth in the FM band and to determine how bright the Earth might appear at meter wavelengths to an observer beyond our own solar system.

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