2Booth et al.
SNRs in Green’s catalog (Green 2019), only 112 (38%) have recorded distances, and many of those are broad estimates
with significant uncertainties1.
One of the most widely applied methods to date for determining distances to SNRs uses the absorption of their
radio emissions by intervening neutral hydrogen gas (HI). Of the 112 SNR distances recorded in Green’s catalog, 51
have been determined by this method. HIbetween an SNR and an observer absorbs the SNR’s emission via the 21
cm (1420 MHz) electron spin-flip transition. This absorption can be used to estimate the distance to the SNR by
placing lower limits on the SNR location. If there is HIabsorption detected in the spectrum of an SNR, we can be
certain that the SNR is some distance beyond the absorbing cloud. Since the frequency of the detected absorption
line represents the motion of the cool HI, the distance to the absorbing HIcloud can be determined through Galactic
kinematics. There may be several absorption features in the spectrum of an SNR, as its emission may pass through
many cool HIclouds; the furthest absorption provides a minimum distance to the SNR (see the top panel of Figure
1; e.g., Schwarz et al. 1980;Foster et al. 2004;Kothes 2013;Tian et al. 2019).
Despite its success, the HIabsorption technique is limited to measuring distances for SNRs that are bright emission
sources (Kothes et al. 2004). While cool HIprimarily absorbs radio waves at 21 cm, warm HIprimarily emits at 21
cm. As a result, the raw spectrum observed towards an SNR usually shows a mixture of continuum emission from the
SNR and line emission from Galactic HI. In addition, cool HIabsorbs the emission from warm HIat the same radial
velocity (HIself-absorption). Unless the SNR has a brightness temperature significantly greater than the background
warm HIemissions, it can be difficult to untangle these different effects.
In order to detect only the absorption of emission from the SNR, removal of the signal contributions from HI
emission and self-absorption may be attempted. To do this, spectra are measured from a position on the SNR and
from a nearby background position off the SNR (see the bottom panel of Figure 1). Assuming that the HIemission
and absorption features in the off-spectrum are identical to those in the on-spectrum, subtracting the off-spectrum
from the on-spectrum yields only the absorption spectrum for the SNR (e.g., Tian et al. 2007;Ranasinghe & Leahy
2018).
There are two problems with applying this background subtraction technique for a low-intensity SNR. First, the
subtraction of two noisy measurements further reduces the signal-to-noise. To improve this situation, the average
emission from a much larger background region can be calculated to reduce the contribution of noise from the off-
spectrum. However, this leads to the second problem: with a larger background region, it is less likely that the
off-source HIbrightness temperature matches what is actually on the source. If there is excess HIemission in the
off-spectrum, then background subtraction will fabricate artificial absorption features. If there is HIself-absorption in
the on-spectrum that is unmatched in the off-spectrum, the additional HIself-absorption features will remain in the
spectrum after subtraction. Therefore, in order to correctly identify HIabsorption of the continuum emission from
the SNR, the SNR must be significantly brighter than the emitting HIalong the line-of-sight (LOS).
We use the novel technique of measuring the absorption of polarized SNR emission in order to circumvent the
ambiguity of HIself-absorption or the emission from small warm HIclouds at the same velocity. All SNRs are
linearly polarized radio sources (via synchrotron emission), while HIemission is not polarized. As a result, if the
linear polarization parameters, Stokes Qand U(hereafter Qand U), are measured from an SNR rather than total
intensity, Stokes I, the excess emission from background HIis eliminated from the spectrum. Since there is no HI
emission in the polarized on-spectrum, there is no need for background subtraction. Consequently, the problems due
to background subtraction are no longer an issue.
Dickey (1997) pioneered the polarized HIabsorption method when he demonstrated HIabsorption of polarized
Galactic extended emission (diffuse synchrotron radiation from relativistic electrons spiraling around interstellar mag-
netic field lines). Kothes et al. (2004) were the first to explore the use of polarized absorption for SNRs. From
observations of the spectra of three SNRs, Tycho’s SNR, DA 495, and G106.3 +2.7, they showed that polarized HI
absorption features tend to be deeper than their counterpart in total intensity and avoid the systematic noise contri-
bution from small warm clouds. They concluded that polarized HIabsorption could be used for any SNR and showed
particular potential for detecting HIabsorption towards weaker sources.
With the distances to a considerable number of Galactic SNRs still undetermined, the development of new techniques
is essential for advancing our understanding of SNRs. Polarized HIabsorption opens up the possibility of reliable
1See https://www.mrao.cam.ac.uk/surveys/snrs/ for the current web version of Green’s catalog