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Processing GOTO survey data with the Rubin Observatory LSST Science Pipelines II: Forced Photometry and lightcurves

Published online by Cambridge University Press:  04 June 2021

L. Makrygianni*
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK The School of Physics and Astronomy, Tel Aviv University, Tel Aviv 69978, Israel
J. Mullaney
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
V. Dhillon
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
S. Littlefair
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
K. Ackley
Affiliation:
School of Physics and Astronomy, Monash University, Clayton VIC 3800, Australia
M. J. Dyer
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
J. Lyman
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
K. Ulaczyk
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
R. Cutter
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
Y.-L. Mong
Affiliation:
School of Physics and Astronomy, Monash University, Clayton VIC 3800, Australia
D. Steeghs
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
D. K. Galloway
Affiliation:
School of Physics and Astronomy, Monash University, Clayton VIC 3800, Australia OzGrav: The ARC Centre of Excellence for Gravitational Wave Discovery, Clayton VIC 3800, Australia
P. O’Brien
Affiliation:
School of Physics and Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
G. Ramsay
Affiliation:
Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK
S. Poshyachinda
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
R. Kotak
Affiliation:
Department of Physics and Astronomy, University of Turku, Vesilinnantie 5, Turku FI-20014, Finland
L. Nuttall
Affiliation:
University of Portsmouth, Portsmouth PO1 3FX, UK
E. Pallé
Affiliation:
Instituto de Astrof’isica de Canarias, La Laguna, Tenerife E-38205, Spain
D. Pollacco
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
E. Thrane
Affiliation:
School of Physics and Astronomy, Monash University, Clayton VIC 3800, Australia
S. Aukkaravittayapun
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
S. Awiphan
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
R. P. Breton
Affiliation:
Department of Physics and Astronomy, Jodrell Bank Centre for Astrophysics, The University of Manchester, Manchester M13 9PL, UK
U. Burhanudin
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
P. Chote
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
A. Chrimes
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
E. Daw
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
C. Duffy
Affiliation:
Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK
R. Eyles-Ferris
Affiliation:
School of Physics and Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
B. Gompertz
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
T. Heikkilä
Affiliation:
Department of Physics and Astronomy, University of Turku, Vesilinnantie 5, Turku FI-20014, Finland
P. Irawati
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
M. Kennedy
Affiliation:
Department of Physics and Astronomy, Jodrell Bank Centre for Astrophysics, The University of Manchester, Manchester M13 9PL, UK
T. Killestein
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
A. Levan
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
T. Marsh
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
D. Mata-Sanchez
Affiliation:
Department of Physics and Astronomy, Jodrell Bank Centre for Astrophysics, The University of Manchester, Manchester M13 9PL, UK
S. Mattila
Affiliation:
Department of Physics and Astronomy, University of Turku, Vesilinnantie 5, Turku FI-20014, Finland
J. Maund
Affiliation:
Department of Physics and Astronomy, University of Sheffield, Sheffield S3 7RH, UK
J. McCormac
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
D. Mkrtichian
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
E. Rol
Affiliation:
School of Physics and Astronomy, Monash University, Clayton VIC 3800, Australia
U. Sawangwit
Affiliation:
National Astronomical Research Institute of Thailand, 260 Moo 4, T. Donkaew, A. Maerim, Chiangmai 50180 Thailand
E. Stanway
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
R. Starling
Affiliation:
School of Physics and Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
P. A Strøm
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
S. Tooke
Affiliation:
School of Physics and Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
K. Wiersema
Affiliation:
Department of Physics, University of Warwick, Gibbet Hill Road, Coventry CV4 7AL, UK
*
Author for correspondence: L. Makrygianni, E-mail: lmakrygianni1@sheffield.ac.uk
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Abstract

We have adapted the Vera C. Rubin Observatory Legacy Survey of Space and Time (LSST) Science Pipelines to process data from the Gravitational-wave Optical Transient Observer (GOTO) prototype. In this paper, we describe how we used the LSST Science Pipelines to conduct forced photometry measurements on nightly GOTO data. By comparing the photometry measurements of sources taken on multiple nights, we find that the precision of our photometry is typically better than 20 mmag for sources brighter than 16 mag. We also compare our photometry measurements against colour-corrected Panoramic Survey Telescope and Rapid Response System photometry and find that the two agree to within 10 mmag (1$\sigma$) for bright (i.e., $\sim 14{\rm th} \mathrm{mag}$) sources to 200 mmag for faint (i.e., $\sim 18{\rm th} \mathrm{mag}$) sources. Additionally, we compare our results to those obtained by GOTO’s own in-house pipeline, gotophoto, and obtain similar results. Based on repeatability measurements, we measure a $5\sigma$ L-band survey depth of between 19 and 20 magnitudes, depending on observing conditions. We assess, using repeated observations of non-varying standard Sloan Digital Sky Survey stars, the accuracy of our uncertainties, which we find are typically overestimated by roughly a factor of two for bright sources (i.e., $< 15{\rm th} \mathrm{mag}$), but slightly underestimated (by roughly a factor of 1.25) for fainter sources ($> 17{\rm th} \mathrm{mag}$). Finally, we present lightcurves for a selection of variable sources and compare them to those obtained with the Zwicky Transient Factory and GAIA. Despite the LSST Software Pipelines still undergoing active development, our results show that they are already delivering robust forced photometry measurements from GOTO data.

Information

Type
Research Article
Copyright
© The Author(s), 2021. Published by Cambridge University Press on behalf of the Astronomical Society of Australia
Figure 0

Figure 1. The region of the sky covered by the GOTO data that we processed using the LSST stack. These data cover the region spanning roughly $-30$ to 90 deg in declination and 15–315 deg in right ascension. This represents roughly 50% of the sky observable at the location of the GOTO prototype on La Palma, Spain.

Figure 1

Figure 2. The distribution of photometric zero-points for the processed frames. The average and standard deviation of this distribution of 22.52 and 0.51. We exclude from further analysis any frames whose zero-points deviate from the average by more than three standard deviations. In further investigation, it was found that these were typically affected by poor observing conditions, including thin cloud cover.

Figure 2

Figure 3. The difference between GOTO photometry measured using the LSST stack and Pan-STARRS PSF photometry, plotted as a function of L-band magnitude. The left-hand plot shows the magnitude difference arising from GOTO aperture photometry, whereas the right-hand plot shows the difference arising from GOTO PSF photometry. Both plots show data arising from all four UTs for a single pointing.

Figure 3

Figure 4. As for Figure 3, but instead showing the difference between LSST stack-measured photometry, and that measured by gotophoto.

Figure 4

Figure 5. Photometric repeatability for 11.16 arcsec aperture photometry as measured with the LSST stack, plotted as a function of L-band magnitude. Each point represents a single reference source within a 4 UT pointing. We use the RMS of the photometry of these sources measured across multiple nights as our measure of repeatability; see Section 4.1 for details. A photometric precision of 0.02 mag (shown as the red line) is achieved for bright (i.e., $m_L\lesssim15$) sources.

Figure 5

Figure 6. As for Figure 5, but now also showing the repeatability of PSF photometry for comparison. While PSF photometry is less precise for the brighter sources, it may be a better choice for fainter sources. We also use the inter-night RMS to estimate the survey depth by using 0.2 mag RMS as an estimate of the 5$\sigma$ detection threshold. This is shown as the horizontal red line at $RMS=0.2 \mathrm{mag}$, which corresponds to L-band survey depths of 18.6 and 19.4 for 11.16 arcsec aperture photometry and PSF photometry, respectively.

Figure 6

Figure 7. Plots used to assess the quality of the uncertainties of our photometry measurements. The top panel shows the robust standard deviation of the quantity of Eqn. 2 as a function of the median magnitude for the GOTO lightcurves from forced photometry. The middle shows the intrinsic scatter of each light curve measured as the robust standard deviation of the magnitude as a function of the magnitude and the bottom panel shows the median error of each light curve as a function of the magnitude. The method evaluates the photometric uncertainties following the method outlined in Suberlak et al. (2017).

Figure 7

Figure 8. Standard deviation of the photometric scatter normalised for the reported photometric uncertainties (left) and intrinsic standard deviation (right) as function of magnitude and coloured by the number of epochs in the lightcurve. There is no obvious correlation for either of them with the number of epochs.

Figure 8

Figure 9. Lightcurves of standard SDSS stars from aperture (upper panels) and PSF (lower panels) photometry. Aperture photometry gives reduced-$\chi^2$ closer to unity, which is what is expected for non-variable stars. Aperture photometry performs better at brighter (i.e., < 15 mag) magnitudes.

Figure 9

Figure 10. Examples of GOTO L-band lightcurves from aperture photometry measured with the LSST stack, presented as phase plots, of periodic variable stars. Also included in these plots are ZTF g-band and GAIA G-band lightcurves, colour-corrected to L-band. These variable stars have period from 0.5 to 6 d and belong to two different classes (top row: Cepheid variables, bottom row: RR Lyraes, the id numbers refer to GAIA ids). GOTO lightcurves contain fewer data points since it has (a) been operating for a shorter period of time than the other surveys and (b) the ZTF in particular has a higher cadence than the GOTO prototype. The shapes of the GOTO, ZTF, and GAIA phase plots are very similar, demonstrating that GOTO will be a valuable resource for time-domain studies of variable sources once it has its full complement of 16 UTs in both the Northern and Southern hemispheres.