Hostname: page-component-89b8bd64d-9prln Total loading time: 0 Render date: 2026-05-10T01:29:20.092Z Has data issue: false hasContentIssue false

An optical daytime astronomy pathfinder for the Huntsman Telescope

Published online by Cambridge University Press:  20 May 2024

Sarah E. Caddy*
Affiliation:
Australian Astronomical Optics, Faculty of Science and Engineering, Macquarie University, Macquarie Park, NSW, Australia School of Mathematical and Physical Sciences, Macquarie University, Sydney, NSW, Australia
Lee R. Spitler
Affiliation:
Australian Astronomical Optics, Faculty of Science and Engineering, Macquarie University, Macquarie Park, NSW, Australia Research Centre in Astronomy, Astrophysics & Astrophotonics, Macquarie University, Sydney, NSW, Australia
Simon C. Ellis
Affiliation:
Australian Astronomical Optics, Faculty of Science and Engineering, Macquarie University, Macquarie Park, NSW, Australia Research Centre in Astronomy, Astrophysics & Astrophotonics, Macquarie University, Sydney, NSW, Australia
*
Corresponding author: Sarah E. Caddy; Email: sarah.caddy@mq.edu.au
Rights & Permissions [Opens in a new window]

Abstract

Observing stars and satellites in optical wavelengths during the day (optical daytime astronomy) has begun a resurgence of interest. The recent dramatic dimming event of Betelgeuse has spurred interest in continuous monitoring of the brightest variable stars, even when an object is only visible during the day due to their proximity to the Sun. In addition, an exponential increase in the number of satellites being launched into low Earth orbit in recent years has driven an interest in optical daytime astronomy for the detection and monitoring of satellites in space situational awareness (SSA) networks. In this paper we explore the use of the Huntsman Telescope as an optical daytime astronomy facility, by conducting an exploratory survey using a pathfinder instrument. We find that an absolute photometric accuracy between 1–10% can be achieved during the day, with a detection limit of V band 4.6 mag at midday in sloan $g,$ and $r,$ wavelengths. In addition, we characterise the daytime sky brightness, colour, and observing conditions in order to achieve the most reliable and highest signal-to-noise observations within the limitations of the bright sky background. We undertake a 7-month survey of the brightness of Betelgeuse during the day and demonstrate that our results are in agreement with measurements from other observatories. Finally we present our preliminary results that demonstrate obtaining absolute photometric measurements of the International Space Station during the day.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - SA
This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-ShareAlike licence (http://creativecommons.org/licenses/by-nc-sa/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the same Creative Commons licence is used to distribute the re-used or adapted article and the original article is properly cited. The written permission of Cambridge University Press must be obtained prior to any commercial use.
Copyright
© The Author(s), 2024. Published by Cambridge University Press on behalf of Astronomical Society of Australia
Figure 0

Figure 1. A sample of detection limits for visual (green), red (red), and short wave infrared (SWIR) (purple) presented in the literature for daytime observations of stars. The data included is from the works of Curtis (1911), Engels et al. (1981), Rork, Lin, & Yakutis (1982), Grishin, Melkov, & Milovidov (2003), Garanin et al. (2017), Kamiński et al. (2021), Shaddix et al. (2021), Zimmer, Ackermann, & McGraw (2021) and this work. Only works that explicitly mention a detection limit are included. Due to the lack of public information surrounding some of the hardware used in daytime observing by various research groups, a reliably reported parameter of telescope aperture is plotted against the detection limit. It should be noted that each of these instruments likely have very different focal lengths and other characteristics, as well as different data reduction methods that may bias results. Three shaded regions in visual magnitudes are also presented, showing rough predicted and observed magnitude lower margins during the day. The brightest stars and planets are visible to most optical systems including the eye (Curtis 1911) during the day and are around $\sim$0th magnitude. The International Space Station has been observed to have a visual magnitude during the day of $\sim$2nd magnitude at zenith (this work). Starlink satellites have been observed in the day up to 3.0 mag (Halferty et al. 2022) at night and up to 2.6 mag during the day (Zimmer, Ackermann, & McGraw 2021). Following the work of Kamiński et al. (2021), most other LEO satellites have a visual magnitude fainter than 8th magnitude.

Figure 1

Figure 2. (A) The Huntsman Telescope remote observing facility located at Siding Spring Observatory, Australia. The telescope consists of 10 Canon 400 mm f/2.8 lenses in an array configured to cover the same field of view of $1.89^\circ \times 1.26^\circ$ with a pixel scale of 1.24”. (B) The pathfinder instrument used to test daytime observing modes for this work consisting of a single lens. The unit is located at Macquarie University Observatory, Sydney, Australia

Figure 2

Figure 3. The observed sky background rate plotted as a function of the exposure time for all filters and targets. The colour bar illustrates the catalogue V band magnitude of the target observed. On the far right, for higher exposure times the image becomes saturated due to the high sky background. To the far left observations are limited by the photon count from the source. Two clear clusters are formed. The lower right are the narrowband filters with much higher exposure times due to their narrow bandwidth, and the upper left are the broadband observations. Exposure times are tuned per every set of observations to ensure that either the image if not over saturated by the target, or by the sky background.

Figure 3

Figure 4. An example airmass plot for the 31st of March 2023, showing the calculated magnitude as a function of airmass for 5 bright reference stars. Observing logs show a clear day, no wind, with tops of $25^{\circ}C$ ($77^{\circ}F$). Each data point is the median of a set of 1 000 exposures for that reference star. The extinction coefficient for this day is found to be 0.27 for $r^{\prime}$ and 0.54 for $g^{\prime}$ with zeropoints of 21.65 and 22.73 respectively. The error bars encapsulate the statistical error of the set of 1 000 observations, and the flat field error in quadrature. The Chi squared values for the linear fit are calculated to illustrate the fit, with a higher Chi squared of 0.93 for $r^{\prime}$ as opposed to $g^{\prime}$. Scatter about an airmass of 1 may be due to dust in the air produced by lawn mowing that observing logs showed to occur close to the observatory at the time of observations.

Figure 4

Figure 5. An example calibration plot for the 10th of March, showing the calibrate mini-Huntsman magnitude as a function of calculate Sloan catalogue magnitude for 5 bright reference stars. Observing logs show a very windy day, passing cloud, with tops of $28^{\circ}C$ ($82.4^{\circ}F$). A violin plot is chosen to illustrate the distribution of calibrated magnitudes over multiple sets of 1000 exposures for each target. The photometric error for this day is found to be 0.05 for $r^{\prime}$ and 0.06 for $g^{\prime}$, around the order of magnitude of the flat field error.

Figure 5

Figure 6. The scintillation index for $g^{\prime}$ and $r^{\prime}$ observations as a function of airmass, plotted together with the calculated theoretical scintillation index using Young’s approximation for the median exposure time for each filter. We find that the $r^{\prime}$ observations are in general agreement with Young’s approximation, however Young appears to overestimate the scintillation for shorter $g^{\prime}$ exposures. However, this could also be due to a bias where by faster exposures times with lower SNR and higher sky Poisson noise in $g^{\prime}$ are less likely to be detected reliably.

Figure 6

Figure 7. The the SNR of the target observation as a function of the sky background rate in $e^{-}/pix/s$. Observations are split up into magnitudes classes of roughly equal sample sizes of $V_{mag} \leq 0$, $0 > V_{mag} < 1.2$ and $V_{mag} \geq 1.2$. The size of the markers indicate the exposure time of the observation. The shape of the marker indicates the bandpass. For the faintest class of stars, the exposure time decreases as a function of the sky background rate. The calculated trend for Poisson sky noise limited observations is plotted, and is found to describe the data in the faintest magnitude class, indicating that observations of stars with $V_{mag} < 1.2$ are Poisson sky noise limited during the day. In contrast, stars in the brightest magnitude class are found to be scintillation noise dominated.

Figure 7

Figure 8. Left panel: The detection probability as a function of the measured FWHM, with colour bar as the Sun altitude in degrees at the time of observation, and the target magnitude is the relative size of the data points. Detection probability is show to decrease with increased FWHM corresponding to the local seeing conditions, and Sun altitude. Right panel: We plot the FWHM as a function of the Sun altitude with detection probability as the colour bar. the We see a relationship between the FWHM and the detection probability, with observations at a detection rate greater than 80% occurring in majority below a FWHM of 4 arcsec, and a Sun altitude of 30 degrees.

Figure 8

Figure 9. Measured sky surface brightness is plotted as a function of Sun separation from the observed target for $g^{\prime}$ and $r^{\prime}$. Grey crosses are V-band filter observations from Nickel & Calderwood (2021). Our observations are in general agreement with the literature, approaching 2 mag/arcsec for Sun separation $>30$ degrees. Sky background surface brightness gradually decreases until falling sharply for Sun altitudes $< 10$ degrees, and Sun separation $> 100$ degrees. The sky is brighter in $g^{\prime}$ than $r^{\prime}$ at Sun separation $< 90$ degrees and $> 40$ degrees. $g^{\prime}$ - $r^{\prime}$ sky colour is explored as a function of Sun separation with the colour bar representing Sun altitude. Data is binned via Sun separation. At Sun separations of $\sim 20$ degrees or higher the sky is redder in colour, and gradually becomes more bluer at larger Sun separations. Sky colours cover a broader range at lower Sun altitudes and larger Sun separations.

Figure 9

Figure 10. Huntsman Pathfinder calculated V band observations plotted in blue, with current Nickel & Calderwood (2021) (observer code NOT) observations during the day in yellow, and during the night in red. In addition, AAVSO (observer code VOL) observations of Betelgeuse are also included for reference in black taken at night. Asymmetrical error bars are calculated to accommodate the flat field error which tends to dominate. A period of consistently poor weather between May and June in the transition from Autumn to Winter resulted in a large gap in our data. Despite this, our results show general a good agreement with both Nickel & Calderwood (2021) and AAVSO observations, with comparable errors.

Figure 10

Figure 11. The trajectory (right panel) and brightness (left panel) of the ISS in $g^{\prime}$ taken by the Huntsman Pathfinder. The error bars are calculated as the photometric error from the calibration stars used on the day, and are flat field corrected. The colour is the target altitude. The target increases in brightness until reaching a maximum of $g^{\prime}$ 1.2 mag. It is lost for a short period during the transit when it drifts out of the field of view, either due to errors in the TLE, the pointing model, or limitations of the mount tracking speed. It is reacquired as it begins the decent, before the mount stops tracking at the meridian due to the mechanical limitations of the equatorial mount.