Issue |
A&A
Volume 514, May 2010
|
|
---|---|---|
Article Number | A27 | |
Number of page(s) | 7 | |
Section | Interstellar and circumstellar matter | |
DOI | https://doi.org/10.1051/0004-6361/200913349 | |
Published online | 06 May 2010 |
Gaussian decomposition of H I surveys
V. Search for very cold clouds
U. Haud
Tartu Observatory, 61 602 Tõravere, Tartumaa, Estonia
Received 25 September 2009 / Accepted 20 January 2010
Abstract
Context. In the previous papers of this series, we decomposed all the H I
21-cm line profiles of the Leiden-Argentina-Bonn (LAB) database into
Gaussian components (GCs), and studied the statistical distributions of
the obtained GCs.
Aims. Now we are interested in separating the ``clouds'' of
similar closely spaced GCs from the general database of the components.
In this paper we examine the most complicated case for our new
cloud-finding algorithm - the clouds of very narrow GCs.
Methods. To separate the clouds of similar GCs, we started with
the single-link hierarchical clustering procedure in five-dimensional
(longitude, latitude, velocity, GC width, and height) space, but made
some modifications to accommodate it to the large number of components.
We also used the requirement that each cloud may be represented at any
observed sky position by only one GC and take the similarity of global
properties of the merging clouds into account. We demonstrate that the
proposed algorithm enables us to find the features in gas distribution,
which are described by similar GCs. As a test, we applied the algorithm
for finding the clouds of the narrowest H I 21-cm line components.
Results. Using the full sky search for cold clouds, we easily detected the coldest known H I
clouds and demonstrate that actually they are a part of a long narrow
ribbon of cold clouds. We modeled these clouds as a part of a planar
gas ring, then deduce their spatial placement and discuss their
relation to supernova shells in the solar neighborhood. Many other
narrow-lined H I structures are also found. We conclude
that the proposed algorithm satisfactorily solves the posed task. In
testing the algorithm, we found a long ribbon of very cold H I
clouds and demonstrated that all the observed properties of this band
of clouds are described very well by the planar ring model.
Conclusion. We also guess that the study of the narrowest H I 21-cm line components may be a useful tool for finding the structure of neutral gas in solar neighborhood.
Key words: ISM: atoms - ISM: clouds - radio lines: ISM
1 Introduction
In earlier papers of this series, we described the Gaussian decomposition of large H I 21-cm line surveys (Haud 2000, hereafter Paper I) and the use of the obtained GCs for detecting of different observational and reductional problems (Haud & Kalberla 2006, hereafter Paper II), for separating thermal phases in the interstellar medium (ISM; Haud & Kalberla 2007, hereafter Paper III) and for studying intermediate and high-velocity hydrogen clouds (IVCs and HVCs; Haud 2008, hereafter Paper IV). A detailed justification for the use of Gaussian decomposition in these studies was provided in Paper III. Observational data for the decomposition came from the LAB database of H I 21 cm line profiles, which combines the new revision (LDS2, Kalberla et al. 2005) of the Leiden/Dwingeloo Survey (LDS, Hartmann 1994) and a similar Southern sky survey (IARS, Bajaja et al. 2005) completed at the Instituto Argentino de Radioastronomia. The LAB database is described in detail by Kalberla et al. (2005). Our method of Gaussian decomposition generated 1 064 808 GCs for 138 830 profiles from LDS2 and 444 573 GCs for 50 980 profiles from IARS.
In Papers II-IV, we used each obtained GC as a single entity, which is independent of all other GCs, and analyzed statistical distributions of their parameters. These results indicated that different structures in the ISM could be recognized as density enhancements in the distribution of GC parameters in the five-dimensional parameter space or that the well-defined GCs with similar parameters at least statistically define the related objects, which share the same physical state in real space. The situation may be more complicated in the cases of heavily blended GCs in emission lines near the galactic plane. These earlier papers also demonstrate the importance of the GC widths, the knowledge of which helps us separate the components, corresponding to different physical structures of the ISM or to the artifacts of the observations, reduction, and the Gaussian decomposition itself. The third point, which is clear from the earlier studies, is that in reality many H I structures, observable in sky, extend to much larger areas than covered by a single beam of the radio telescope. This means that some GCs of the neighboring profiles may represent the features of a similar origin and that they are not independent of the others, so may be grouped together to represent larger structures.
In the present paper, we start studying these similarities and relations between the GCs, by defining clouds of similar GCs, which may (but need not) describe the real gas concentrations in the real space. In doing so, we must keep in mind that there are no precise definitions of the terms such as ``cloud'', ``clump'', or ``core'' (Larson 2003), and the physical reality of the clumps, found by different authors, has been a matter of controversial debate since the presentation of the first systematic attempts to identify any kind of gas clumps. Nevertheless, many papers have been devoted to the study of clouds, clumps, and cores in the ISM.
As the structure in molecular clouds determines, in part, the locations, numbers, and masses of newly formed stars, much effort has been invested in characterizing this gas. The clumpy substructure of molecular clouds was first identified by eye (Blitz & Stark 1986; Carr 1987; Loren 1989; Nozawa et al. 1991; Lada et al. 1991; Blitz 1993; Dobashi et al. 1996). However, as a power-law mass spectrum predicts an increasing number of smaller and smaller clumps, confusion is usually the limiting factor in clump identification by eye. It is thus highly desirable to use automated clump-finding algorithms in the analysis of observed data, as the use of an algorithm allows the structure to be analyzed in a consistent and stable way (Kramer et al. 1998).
The two applications that have the most shaped molecular line astronomy are the clump identification algorithms GAUSSCLUMP by Stutzki & Güsten (1990) and CLUMPFIND by Williams et al. (1994). GAUSSCLUMPS uses a least square fitting procedure to decompose the emission iteratively into one or more Gaussian clumps. CLUMPFIND associates each local emission peak and the neighboring pixels with one clump (similar to the usual eye inspection procedure). Although the basic concept of both algorithms is quite different, they give consistent results for the larger clumps, when used on the same data (Williams et al. 1994). With H I data Thilker (1998) has used an algorithm, somewhat similar to GAUSSCLUMPS, and applied it to look for H I bubbles blown by supernovas in external galaxies. The method, similar to CLUMPFIND, was used by de Heij et al. 2002 to automatically search for compact high velocity clouds (HVCs) in the Leiden/Dwingeloo Survey.
Later Nidever et al. (2008) have used the Gaussian decomposition of the LAB profiles with the algorithm created according to the description of our decomposition program in Paper I. The obtained GCs are then used to disentangle overlapping H I structures. They stress that using GCs makes it possible to distinguish different H I filaments even when they are overlapping in velocity. They state that in these situations the GCs trace structures that are real, and they may even contain physical information about the structures. They were successful in tracking tenuous structures through rather complicated environments, even though the decomposition of those environments likely carries no physical meaning. The results were used to study the origin of the Magellanic Stream and its leading arm.
We would like to move a step further and use an automatic computer program for finding different continuous H I features in the full decomposition of the LAB database. In the next section, we give a brief description of the algorithm for finding coherent structures in the large database of GCs. The details of our algorithm are published in [arXiv:1001.4155v1]. Here we argue that the most complicated case for our cloud-finding approach are the clouds of the narrowest GCs, and concentrate our attention on the test with such cold clouds. Therefore, as the first step we have applied the program for the full sky search of the coldest H I clouds in the Galaxy, which could be identified using the LAB data. Then we argue that this search has rediscovered some of the coldest clouds observed so far in H I emission, and demonstrate that these known clouds actually constitute only a small part of a considerably larger coherent structure. Finally, we describe this structure with the help of a planar ring model, deduce its location in the space, and discuss the possible relations with some supernova shells in the Local Bubble (LB).
However, during all these studies we must keep in mind that the widths of such narrow GCs, as used in this paper, most likely are not correct representations of the actual widths of the underlying H I 21-cm emission lines. Because of both the finite optical depth of the lines and the velocity resolution of the LAB survey, the GC widths used here are mostly the upper limits for the actual line widths. Therefore, they cannot be used to the study physical properties in the clouds, but as the actual lines are even narrower than the corresponding GCs, we may still state that we are looking for very narrow lines and very cold gas clouds.
2 The cloud-finding algorithm
The task of finding the clouds of similar objects belongs to cluster analysis. As in previous papers of this series, we have studied some distributions of GCs, considering all components more or less independent of each other, so it is now natural to follow some agglomerative (bottom-up) hierarchical clustering procedure. If we are looking for clouds whose parameters vary smoothly from one point to another, the most appropriate algorithm seems to be single-link clustering. We add to the existing cluster a new element, which is the closest to at least one of the elements of this cluster. However, we faced some problems with direct use of the single-link clustering.
In the Galaxy, H I has a rather complicated spatial and kinematic structure, so that the Gaussian decompositions of the profiles, particularly near the galactic plane, may be rather complicated and contain many different GCs per profile. Running the preliminary versions of our cluster identification program demonstrated that, without applying special restrictions, one dominating cloud started to emerge around the galactic plane from the first steps of the merging process. Finally only these H I structures were distinguishable, whose properties differ very strongly from those of general ISM. We would instead like to achieve opposite results: to separate all the pieces of more or less coherent structures and follow them as close as possible to other structures, but not to merge probably different features. To achieve this, we decided that every GC of the profile must represent a different feature of the gas in a particular sky position.
For example, in HVCs we often get two GCs in the same profile at nearly the same velocity, and most likely they both describe the same physical cloud, but the narrow GC represents the properties of the gas in compact cold cores, and the wider component describes the gas in the more extended warmer envelope of the cloud (Kalberla & Haud 2006; Paper IV). We decided to consider such features as different entities of ISM and therefore to apply a restriction that every cloud of GCs may only contain one component from each profile. In this way, if in some problems we need to consider ``cores'' and ``envelopes'' together, we may join corresponding clouds for this particular task, but if we allow them to merge from the beginning, it would be harder to separate out different subclouds for some other studies.
One more problem emerged at later stages of the merging of GCs into clouds. By using a pure single-link clustering algorithm, we sometimes found the cases where two clouds with rather different average properties merged, as they touched each other at some point on their outer perimeter. As this was undesirable, we added a test of the similarity of global properties of the merging subclouds, and actually merged them only in those cases where this similarity was above a predefined limit.
Besides the algorithm of joining different GCs into clouds, an
important step in any cluster-finding process is also the
selection of a distance measure, which will determine how the
similarity of two elements is calculated. After testing some
possibilities, we decided to quantify the dissimilarity of the GCs
Ei and Ej of neighboring profiles with the parameter
where the GCs E are given by
and T is the height of the component at its central velocity V, and W determines the width of the GC. Integrating and for computational convenience applying the transformation

The parameter S, as defined by Eq. (3), compares the values of two Gaussian functions at all possible velocities and corresponds to the natural human understanding of the similarity of two curves: they are similar when they are close to each other everywhere. The parameter S = 0, when two GCs have exactly the same values of their parameters and for increasingly different components

It is easy to see that this definition also compensates for uncertainties in the determination of the GC parameters, as discussed in Sect. 4.2. of the Paper I. For example, in the presence of noise our decomposition program gives the most unreliable values for the central velocities and widths for the widest GCs (component D in Fig. 10 of Paper I). However, when the line widths become larger, the differences in central velocities and also in widths become less important in the first addend of Eq. (3). Therefore, we may conclude that our dissimilarity measure treats the observed lines of different width with more or less the same precision. This is good for comparing two independent GCs, but may pose problems for the clustering, because all natural gradients in parameter values become increasingly important for narrower components. It may make the detection of small, bright, but cold clouds of H I rather problematic. Therefore, we decided to test our approach with the narrowest GCs found in the decomposition of the LAB.
3 Search for very cold clouds
To our knowledge, the coldest clouds in the Galaxy, found so far
in H I emission, are the two gas concentrations at
near-zero velocity around
and
,
discovered by Verschuur (1969)
and afterwards studied in more details by Verschuur & Knapp
(1971) and Knapp & Verschuur (1972). Later, the
third cloud around
was added to the
first two by Heils & Troland (2003), and one of the
recent detailed studies of these clouds is the one by Meyer et al.
(2006). They observed the interstellar Na I D1 and
D2 absorption toward 33 stars, derived a cloud temperature of
,
and placed a firm upper limit of
on the distance of the clouds. This distance
corresponds to the upper limit of the linear size of the clouds of
about
.
Redfield & Linsky (2008) interpret
these clouds as the result of the collision of the warm
high-velocity Gem Cloud with the slower moving Leo, Aur, and LIC
clouds in the Local Interstellar Medium (LISM). At the same time,
the properties of the clouds also seem to be similar to the
temperatures (mostly
)
and to dimensions
(in parsec scale) of numerous H I self-absorption features,
found near the galactic plane (e.g. Gibson et al. 2000;
Dickey et al. 2003; Kavars 2005; Hosokawa &
Inutsuka 2007). Our interest in the subject is to test
whether the clustering algorithm finds these clouds.
For this test we first constructed the dendrogram for all GCs in
our decomposition and inspected the resulting clouds for different
values of the cutting level of the dendrogram. From this
inspection, we chose the value
for the
final cutting level. In this way we obtained 94 874 clusters of
GCs, and 236 306 components remained detached from the others.
The largest cloud (12 585 GCs) in the obtained list corresponds
to a relatively smooth warm neutral medium at high galactic
latitudes, but the list also contains many very small clouds of
2-3 GCs each (the cluster size distribution follows the power law
with a slope of about 1.9). As Verschuur & Knapp (1971)
have estimated that their cool clouds have diameters of at least
,
we are not interested in the smallest clouds in our
list, and in the following, we only consider the clouds that
contain at least 7 GCs (in LAB one profile represents an area of
0.25 square degrees and 7 profiles cover the area, corresponding
to the cloud with the diameter of
). In our list, there
are 21 224 clouds of this size.
![]() |
Figure 1:
The velocities, line-widths, and brightness
temperatures in clouds of at least 7 GCs, compiled by our
clustering algorithm. Shown are the objects for which the
mean GC height is |
Open with DEXTER |
To search for the coldest clouds in the list, we must apply some
additional selection criteria. First of all, we are looking for
clouds that consist of relatively narrow GCs. In Paper III, we
demonstrated that the mean line-width of the H I 21-cm
radio lines of the cold neutral medium of our Galaxy is
.
Therefore, the gas, with
,
may already be considered as a very
cold gas, so we look for the clouds where the mean width of the
GCs is below this limit. In Paper II, we also demonstrated that
many weak and/or very narrow GCs do not represent the actual
H I emission of the Galaxy, but are more likely caused by
observational noise or radio interferences. Here we are not
interested in these GCs, so we apply the selection criteria, given
by Eqs. (4) and (5) of Paper II. However, now we do not apply these
criteria to single GCs, but to the clouds obtained from our
clustering process.
From Eqs. (4) and (5) of Paper II, it follows that the narrowest GCs,
which most likely represent the galactic H I, have the
heights
.
Therefore, we consider only those
clouds for which the mean height of their GCs is
.
At first sight, a similar selection (
,
corresponding to Eq. (4) of Paper II) may
also be applied to the width of the GCs. However, we are looking
for clouds with the narrowest GCs, and some of the real lines may
be even narrower than interferences with
.
Therefore, as this selection may reject not only the
interferences, but also a considerable amount of GCs that are the
main interest in our study, this selection cannot be applied
directly. At the same time, the selection rule given by Eq. (4) of
Paper II applies only statistically, and it turned out that better
results can be obtained by rejecting the clouds, for which more
than half of their GCs do not satisfy Eq. (4) of Paper II.
Nevertheless, some confusion with the interferences still remains.
After applying all the described selection criteria, we had a list
of 1 380 cold clouds. However, when looking at these clouds, we
saw that the clouds with the highest velocities (concentrated
around +50 and
)
were only located in
a very narrow band around the galactic plane (all at
,
most at
). We have stressed several times
that the Gaussian decomposition gives relatively unreliable
results in these regions, and the corresponding GCs are probably
not directly related to the physical properties of the ISM.
Therefore, we decided to also reject those clouds by applying the
requirement
on the mean
velocities of the clouds. In this way, we rejected 44 more small
clouds. All remaining clouds are presented in Fig. 1.
When applying the described selection criteria on clusters,
obtained with different values of the cutting level,
,
of the dendrogram, we found that for
the number of GCs in the selected clouds
increases rapidly. For
,
the
pictures similar to Fig. 1 remain nearly unchanged with
only a slight maximum in the number of GCs for
.
After
,
the number of GCs starts to
decrease, because gradually wider and wider GCs are linked to the
existing clouds and the average line widths of clouds grow above
our selection limit. For Fig. 1, we chose the value of
,
which gave the highest number of GCs in the
selected clouds.
4 Verschuur's clouds
![]() |
Figure 2:
The velocities, line-widths, and brightness
temperatures of the clouds in the region of the observable
part of the ring. Shown are the objects, represented by at
least 7 GCs, for which the mean GC width
|
Open with DEXTER |
From Fig. 1, we can see that the cold clouds around
,
,
and
,
mentioned at the beginning of the
previous section, are clearly visible. Moreover, in this figure
these clouds seem to be part of a more extended narrow string of
clouds, covering the sky about
from
to
.
This is in good agreement with the remark by Heils &
Troland (2003) that other narrow H I 21-cm emission
lines can be found in the extended region around the clouds,
studied in their paper. Nevertheless, they limited their interest
to the longitude interval of
and
report the broken ribbon of cold H I gas stretching over
across the constellation Leo.
These clouds are plotted in Fig. 2 in more details. To
better separate them from other features in the same sky region,
we have used even more severe selection criteria here (
,
), compared to those for
Fig. 1. However, because the noise GCs are effectively
removed from the data also by using only clouds of 7 or more GCs,
we dropped the requirement
to increase the
sensitivity. The selection criteria, used for Fig. 1,
led to the dendrogram cutting level
.
Now we
changed the criteria and the considerations, described above, give
somewhat higher value
.
As a result, we
obtained a chain of clouds, which seems to follow some arc and
which is well populated in its higher galactic longitude half and
more opened at lower longitudes.
We can see a clear velocity gradient along this ribbon of clouds
with the average velocities of the clouds increasing by about
per arc length. A similar, but a much
weaker gradient also holds for the line widths: the average FWHM of the clouds increases by
from the higher
galactic longitudes towards the lower longitudes. It also appears
that the clouds tend to be brighter near their centers than in
outer regions, which is expected behavior for real gas clouds. In
this way, while the lower longitude part of the string of clouds
is also interrupted in some places by voids, the coherence of its
characteristics strongly indicates that it is really the same
physical feature. It remains questionable whether the clouds at
and
also belong
to the same structure because they deviate from the others
considerably on the sky or in velocity. Therefore, we did not use
them in the following discussion.
The observed structure is so smooth that it seemed interesting to
try to model it. Since arced shapes often hint at circular
structures, when seen under some angle to their plane, we decided
to model this string of clouds and their velocities as a partial
gas ring somewhere in space, which may move relative the local
standard of rest (LSR) as a whole and also rotate around its
center and expand away from this center. We found that such a
model describes both the apparent location of the clouds on the
sky and their observed velocities very well. According to this
model, the center of the ring is located in the direction
,
its apparent major
axis is inclined by
to the galactic plane, and
the angle between the ring plane and the line of sight to its
center is
.
The radius of the ring is seen
under the angle of
along the apparent major
axis of the observed structure. The ring as a whole moves with the
velocity of
in the direction
and rotates
clockwise with the velocity of
,
and its expansion speed is
.
As
errors in these parameters are given the 99.73% confidence limits
obtained from the bootstrapping.
The projection of the model ring onto the sky is shown with a line
in the first (V) panels of Figs. 1 and 2.
The color of the line corresponds to the line-of-sight velocity of
each ring point. The fit of the model to the observed gas
velocities is shown in the lower right part of Fig. 2.
From Fig. 1, we can see that actually the same structure
seems to continue even beyond the lower latitude border of
Fig. 2, and it can be followed down to about
.
However, this continuation of the ring
is rather sparsely populated with relatively small clouds and is
located near the galactic plane, where the Gaussian decomposition
cannot be considered to be reliable. Therefore, we do not discuss
this continuation in more detail than just mentioning that, when
the parameters of the ring were estimated only from a
segment of the whole ring (as seen from the ring center and
indicated in the lower right panel of Fig. 2), in total
the visible part of the ring may extend to nearly half
(
)
of the full circle. For the other half there seems to
be no good candidates for the same structure. But, of course, the
location of the model ring is also uncertain in these regions.
5 The ring in space
In most H I profiles, the emission, corresponding to the clouds under discussion, appears as a very narrow and relatively strong line, not seriously blended by a broader-velocity, lower-intensity emission component. Therefore, it may seem to be easy to derive some estimates for the physical conditions inside these clouds from the parameters of our GCs. Unfortunately, as briefly mentioned in the Introduction, this is not true. Already, Verschuur & Knapp (1971) demonstrated that the shapes of these narrow emission lines are actually not Gaussian, but they are considerably influenced by saturation. They derived the spin temperature by assuming the optical depth to be a Gaussian function of the frequency and fitting the observational data to the equation of transfer. We cannot even use this path, since the velocity resolution of the LAB data is more than 10 times lower than that of the data used by Verschuur & Knapp (1971), leaving the actual line-shapes mostly unresolved.
Nevertheless, we decided to take a further step by obtaining at least some preliminary estimate for the distance of the ring. In doing so, we followed the procedure described by Haud (1990). These estimates are based on the assumption that a correlation exists in cold H I clouds between the cloud's internal velocity dispersion and its linear dimensions, similar to the one observed for molecular clouds (Larson 1981 and many others since then). We do not discuss all these questions here, related to the existence or meaning of such correlation, but use it just as a possible tool, which may or may not give some acceptable results. We followed the same procedure exactly as described in Haud (1990) with the only exception that we did not correct the LSR velocities of the clouds to the galactic standard of rest (GSR), as it is most likely unjustified in this case. Instead, we removed the large-scale velocity gradients and projection effects in the ribbon clouds using our ring model. In this way, we obtained the distance estimates for all ring clouds and, with our model of the ring, converted them to estimates of the distance of the ring center.
As expected, we got fairly scattered results, but in general, the
distance estimates of individual clouds agreed with our ring
model, which indicates that the lower longitude tip of the band of
clouds is located about twice as far from us as the higher
longitude tip. As the scatter of the obtained estimates was
considerably higher for estimates, based on smaller (covering
fewer gridpoints of LDS observations) clouds than for those based
on larger clouds, we decided to accept the weighted average of all
determinations for the distance of the ring center and to use as
weights the number of GCs in each cloud. In this way, we obtained
a distance estimate of
.
The error
estimate corresponds only to the scatter of individual distance
estimates and does not account for uncertainties in the ring model
or in the method, used for obtaining these distances. To this
distance corresponds the linear radius of the model ring of
and the distance of the Verschuur's cloud A of
,
which is in good agreement with the upper
distance limit (
)
for this cloud, as established
by Meyer et al. (2006).
Of course, a number of questions remain with such a model. First
of all, why model this structure as a planar ring of gas clouds,
when most processes, which may give the expansion velocities,
obtained for this ring more likely have spherical symmetry?
Moreover, when the ribbon of gas clouds covers nearly
in
the galactic longitude, this corresponds in our model only to
along model ring itself. This means that we do not
actually know anything about most of the ring, therefore its
parameters may contain large systematic errors. Also, the distance
estimates are based on rather arbitrary assumptions, and they are
quite uncertain. Because the GCs most likely overestimate the
widths of the actual underlying H I lines, they must be
considered as upper limits for the corresponding actual distances.
Nevertheless, even such a model demonstrates the coherence of the
observed clouds well, because it seems to give some indication of
possible continuation of the structure even beyond the region
studied here, and it is interesting to see that the distance
estimates of the individual clouds and the ring model generally
agree with respect to the orientation of the gas band in
3-dimensional space. Moreover, we have seen that the observed
behavior of the gas stream at lower longitudes may be understood
in the framework of this model: in these regions the distance of
the clouds from the Sun increases so they apparently become
smaller. As we have selected only relatively large clouds from our
clustering results (at least 7 GCs in each cloud), we may lose
most of the apparently smaller ones from our view. Therefore,
beyond about
and the distance
,
the stream becomes fragmentary, and we can only
observe some seemingly small clouds, which actually may have
relatively large linear dimensions and line widths. As here we can
no longer see the really smallest and coldest clouds, this may
explain the increase in the average observable line widths in this
region. But why then does the stream terminate so abruptly at its
other end? This happens practically at the nearest point of the
ring to the Sun.
Wolleben (2007) has proposed a model for the north polar
spur (NPS) region. This model explains the results of the Dominion
Radio Astrophysical Observatory Low-Resolution Polarization Survey
(Wolleben et al. 2006), and the model consists of two
synchrotron-emitting shells, S1 and S2. The same model shell S1
was used by Frisch (2009) to explain the direction of the
interstellar magnetic field at the heliosphere, the polarization
of light from nearby stars, and the kinematics of nearby clouds.
We studied the mutual placement of these shells and our ring, and
found that the ring intersects with the shell S2 in the direction
at the distance of
from the Sun. This position matches the beginning of our band of
clouds exactly, and the result is nearly independent of the fairly
indefinite determination of the linear size of the ring. Farther
to the higher longitudes, the ring continues inside the S2, and
the ring clouds are probably destroyed by the shell. The ring
leaves the shell at
at the distance
of
from the Sun. As with the lower longitude end
of the gas stream, we may expect that the ring clouds, even if
they exist there, are mostly unobservable at these distances.
A problem with this explanation of the observability of the ring
clouds is that the ring intersects the S1 shell at
,
,
,
but is still
observable on both sides of this point. Maybe only a slight
disturbance of the velocities of the ring clouds can be seen in
this region. However, the explanation of the different behaviors
of the ring clouds at the intersections with two different shells
may lie in the different ages of these shells. According to
Wolleben (2007), the S1 shell is about 6 million years old
and only observable as a small part of ``New-Loop'' in the
southern galactic hemisphere. The S2 shell is 1-2 million years
old and seems to be much more active since it is responsible for
the well known NPS. Therefore, we may expect that the S1 shell is
no longer energetic enough to destroy the ring clouds, as they are
destroyed by S2. By arbitrarily using the standard model for the
kinematic age of stellar wind bubbles (Weaver et al.
1977), we may estimate that the age of the ring itself is
about 2.5 million years, comparable to the age of the S2 shell.
However, the physical mechanisms responsible for producing such
cold clouds in the environment of the hot LB are still poorly
understood (Stanimirovic 2009).
6 Conclusions
So far we have decomposed the LAB database of H I 21-cm line profiles into the GCs (Paper I) and studied the statistical distributions of the obtained components (Papers II-IV). These distributions have revealed several interesting structures, but have given only the probabilities with which some particular GC may belong to one or another structure. In this Paper (V), we have proposed an algorithm for grouping similar GCs. In this way, we free ourselves from the need to study each GC separately, and we may expect that all the GCs of the ``cloud'' of similar components have the same nature. It may also be possible to obtain some additional physical information from the shapes and sizes of such clouds.
As a test problem, we considered the separation of clouds of the narrowest GCs as based on the preliminary considerations, this may be the hardest problem for our algorithm. We demonstrated that the algorithm easily found the coldest known H I clouds discovered decades ago by Verschuur (1969). As expected, the tests indicate that, depending on the cutting level of the clustering dendrogram, our approach may divide some larger clouds into separate, more coherent substructures, but it hopefully avoids the merging of unrelated features. This behavior was intentional, as it seems more appropriate to study a larger number of clouds where each represents a certain type of line features than to have fewer clouds that may mix GCs of different natures into one.
We also found that Verschuur's clouds form only a small part of a
much longer ribbon of presumably very cold clouds covering the sky
about
.
As the gas velocities and line widths vary along
this ribbon, we decided to model the whole structure as a part of
a planar gas ring that may move in space as a whole and also
rotate around and expand away from its center. Such a model
represented the observed properties of the gas stream very well
and indicated that the ring center must be located at a distance
of
from the Sun in the direction
.
The ring radius is
about
,
its apparent major axis is inclined by
to the galactic plane, and the angle between
the ring plane and the line of sight to its center is
.
The ring as a whole moves with a velocity of
in the direction
,
it rotates clockwise with the
velocity of
,
and its expansion
speed is
.
In the framework of
such a model, the apparent gradual weakening of the ring clouds at
the lower longitude tip of the stream is explained by increasing
distances between the Sun and the ring clouds in this region, and
the abrupt end of the stream at the higher longitude part is
caused by the intersection of the ring with the S2 supernova shell
from the model by Wolleben (2007).
In many respects most of other clouds, seen in Fig. 1, are somewhat different from the ring clouds: lines are slightly wider, velocities less coherent over the structures etc. We did not attempt to model these features, but because the line widths of these clouds are also small, they must be relatively cold clouds, so not very large spatially. As these clouds of presumably small linear dimensions cover fairly large areas on the sky, they probably cannot be located very far from the Sun; therefore, the studies of such narrow-lined clouds may give useful information about the gas in the solar neighborhood. Usually this gas is studied through corresponding absorption lines, which allow estimation of physical conditions in the local gas. The H I 21-cm emission line is less useful in this respect, but may still be usable for large-scale surveys to find out possible interesting features in the local neighborhood.
As a result, we may state that the ring clouds seem to be a unique feature on the sky. Most likely they are the coldest clouds observable in the H I 21-cm emission line. Also, slightly warmer clouds (clouds with slightly wider 21-cm emission lines) may be related to local gas structures inside or near the LB. Some properties of these clouds may be similar to those with the H I self-absorption features, observed predominantly near the galactic plane, where our approach to the emission data is most likely not applicable, but in this paper we have not studied this in enough detail to make firm statements.
AcknowledgementsThe author would like to thank W. B. Burton for providing the preliminary data from the LDS for program testing prior to the publication of the survey. A considerable part of the work on creating the decomposition program was done during the stay of U. Haud at the Radioastronomical Institute of Bonn University (now Argelander-Institut für Astronomie). The hospitality of the Institute staff members is highly appreciated. We thank Drs. I. Kolka, E. Saar, P. Tenjes, and K. Annuk for fruitful discussions. We also thank our anonymous referee, whose suggestions improved the clarity of the paper. The project was supported by the Estonian Science Foundation grant no. 7765.
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All Figures
![]() |
Figure 1:
The velocities, line-widths, and brightness
temperatures in clouds of at least 7 GCs, compiled by our
clustering algorithm. Shown are the objects for which the
mean GC height is |
Open with DEXTER | |
In the text |
![]() |
Figure 2:
The velocities, line-widths, and brightness
temperatures of the clouds in the region of the observable
part of the ring. Shown are the objects, represented by at
least 7 GCs, for which the mean GC width
|
Open with DEXTER | |
In the text |
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