A&A 420, 975-986 (2004)
DOI: 10.1051/0004-6361:20041124
F. McGroarty - T. P. Ray
Dublin Institute for Advanced Studies, 5 Merrion Square, Dublin 2, Ireland
Received 29 January 2004 / Accepted 26 March 2004
Abstract
Previous studies of young stellar objects (YSOs) have uncovered a number of associated parsec-scale
optical outflows, the majority of which are driven by low-mass, embedded Class I sources. Here we
examine more evolved Classical T Tauri stars (CTTSs), i.e. Class II sources, to determine whether these
are also capable of driving parsec-scale outflows. Five such sources are presented here - CW Tau,
DG Tau, DO Tau, HV Tau C and RW Aur, all of which show optical evidence for outflows of the order of
1 pc (24' at the distance of Taurus-Auriga). These sources were previously known only to drive
"micro-jets'' or small-scale outflows
1
in length. A parsec-scale outflow
from a less evolved source (DG Tau B) which was noted in the course of this work is also included here.
Examination of the five newly discovered large-scale outflows from CTTSs shows that they have
comparable morphologies, apparent dynamical timescales and degrees of collimation to those from less
evolved sources. There is also strong evidence that these outflows have blown out of their parent
molecular clouds. Finally we note that the "fossil record'' provided by these outflows suggests their
sources could have undergone FU Orionis-type outbursts in the past.
Key words: ISM: Herbig-Haro objects - ISM: individual objects: CW Tau - ISM: individual objects: DG Tau - ISM: individual objects: DO Tau - ISM: individual objects: HV Tau C - ISM: individual objects: RW Aur
Herbig-Haro (HH) objects are the optically visible tracers of mass outflow from YSOs and are
therefore ultimately powered by accretion (Cabrit et al. 1990; Hartigan et al. 1995). Over the years many bipolar HH
outflows have been observed and most were found to be driven by embedded, low-mass sources of
1
. Initially it was assumed that their lengths were only a fraction of a parsec, however the
discovery of a
1.4 pc long outflow from RNO 43 (Ray 1987) hinted that this may not always be
the case. In the mid 1990's it was realised that many of these outflows can have projected lengths much
greater than 1 pc (Bally et al. 1996; Reipurth et al. 1997; Eislöffel & Mundt 1997), reaching up to
11 pc. Some well known
examples are the HH 34 outflow consisting of HH 33, HH 40, HH 85, HH 126, HH 34N, HH 34, HH 34X,
HH 173, HH 86, HH 87 and HH 88 which is 3 pc in projected length (Bally & Devine 1994); the 5.9 pc long
HH 401, HH 1, HH 2 and HH 402 outflow (Ogura 1995); and the HH 113/HH 111/HH 311
outflow at 7.7 pc in length (Reipurth et al. 1997).
It is not surprising that such outflows can attain these lengths when we consider that they have tangential velocities of between 50-200 km s-1 (Devine et al. 1997; Reipurth et al. 1997) and the outflow phase, for even (low-mass) Class I sources, lasts at least 105 years. In reality, it should be expected that most will attain parsec-scale lengths. The main observational hindrance in the past to observing them was the relatively small fields of view offered by most CCD cameras. With the advent of large CCD mosaics more and more parsec-scale outflows have been discovered.
The morphology of parsec-scale outflows yields valuable information about their driving
sources. They are, in effect, a fossil record of the mass-loss history of their source over their
dynamical timescales (
103 to
105 yr). They suggest, for example, quiescent
phases between periods of violent mass ejection that give rise to the large HH complexes we see today.
The morphology of an outflow can also indicate whether it is precessing and, if so, the rate of
precession.
As mentioned earlier many of the parsec-scale outflows that have been observed to date are driven
by young, Class I, low-mass YSOs. The classification scheme used here is based on the shape of
the spectral energy distribution (SED) of the YSO from 10
m to 100
m (Lada 1987; Lada & Wilking 1984). The
SED of a YSO can be modelled as an approximate blackbody with an infrared excess longwards of 2
m
due to circumstellar dust and gas. The infrared excess is very strong in the young, embedded Class I
sources and is almost non-existent in the most evolved Class III sources. Here we observed a number
of Class II low-mass sources - CTTSs. These CTTSs were not previously associated with
parsec-scale outflows; in fact many were only known to drive "micro-jets'' of the order of
5
to 40
(
0.03 pc at a distance of 140 pc to the Taurus-Auriga Cloud).
Although outflows from these more evolved sources are not nearly as spectacular as those from Class I
YSOs, their sources are no longer surrounded by significant amounts of dust and so their outflows can
be traced right back to the origin. These Class II sources are still actively accreting and ejecting
matter, albeit at rates 10-100 times smaller than Class I sources (Hartigan et al. 1995). In this
paper, we present a number of parsec-scale outflows from CTTSs and we investigate whether these
CTTSs show evidence for having undergone FU Orionis-like outbursts, based on the fossil record of their
outflows.
Details about the observations are given in Sect. 2. In Sect. 3 we report the discovery of parsec-scale outflows from five CTTSs in the Taurus-Auriga Cloud, at a distance of 140 pc (Wichmann et al. 1998; Elias 1978). We also include serendipitous observations of a parsec-scale outflow from a less evolved Class I source. These results are discussed in Sect. 4 and our conclusions are presented in Sect. 5.
Our data was acquired using the Wide Field Camera (WFC) on the 2.5 m Isaac Newton Telescope at
El Observatorio del Roque de los Muchachos (La Palma, Canary Islands). The WFC consists of four
thin-coated EEV CCDs each with
,
15
m
15
m pixels. One pixel
projects to 0
33 on the sky. Three of the CCDs are positioned from north to south with their long
axes adjoining. The fourth is attached to the west to form a square (34
2 wide) with its
northwestern corner missing.
Our images were taken during two separate observing runs, the first between the 10th and
13th of February 2001, and the second between the 24th and 27th of November 2003. HH objects were identified using a number of narrowband emission line filters:
H
(
= 6568 Å,
Å) and
[SII](
Å,
Å). To distinguish HH emission from reflection nebulosity, we also took broadband images in I and V. Seeing in the images taken in February 2001 was moderate at
1
-2
as measured from the images. The seeing in the November 2003 images was better
at 0
9-1
1. Exposure times for the narrowband and broadband images were typically 30 and
10 min respectively. The data were reduced using standard IRAF reduction procedures.
The sources observed here are CTTSs with previously known "micro-jets'' or short outflows of
1
.
All are in the Taurus-Auriga cloud, chosen for its abundance of CTTSs. Seven such
sources were observed, with 5 of them - CW Tau, DG Tau, DO Tau, HV Tau C and RW Aur - revealing
extended outflows of the order of 1 pc. No extended optical emission was found in the UY Aur and
DP Tau outflows.
Table 1: Positions of the new HH objects found in this survey and their probable sources.
CW Tau has a spectral type of K3 (Cohen & Kuhi 1979), with
and
(Gomez de Castro 1993). A "micro-jet'' (HH 220) propagating southeast from
this source was discovered in optical images by Gomez de Castro (1993), with a gap of
1
3
between the source and the jet. A full opening angle of 3.3
is derived for this blueshifted jet
at 3
from the source (Dougados et al. 2000). Long-slit spectroscopic observations by
Hirth et al. (1994) showed the outflow to extend at least 4
-6
on either side of the
source. The blueshifted HH 220 outflow is at a position angle (PA) of 144
2
with respect to CW Tau (Dougados et al. 2000; Gomez de Castro 1993) and we estimate the redshifted jet to be at
329
with respect to CW Tau from the [SII] images of Dougados et al. (2000).
Our wide field images of the region around CW Tau (Fig. 1) reveal that this outflow is
much more extended than just the HH 220 bipolar jet - see Table 2 for details of
the newly discovered objects in the CW Tau outflow. Two knots are found to the south of CW Tau
at 22
(HH 826 A) and 1
27 (HH 826 B). HH 826 A is only seen in [SII] emission while
HH 827 B is seen in both [SII] and H
.
Both are at a PA of
153
with respect to
the source and are reasonably well aligned with the blueshifted HH 220 jet. Further out at 6
1 is
HH 827 at a PA of 184
with respect to CW Tau. Precession of the outflow may explain this
directional change. HH 827 consists of a bright knot with a trail of emission stretching to the
northeast and a fainter trail of emission to the southwest (see Fig. 3) and is
much brighter and more extended in H
than in [SII]. The total length of this object in
H
is
1
8. It is possible that HH 827 is not driven by CW Tau in which case
IRAS 04113+2758 and IRAS 04112+2803 to the northeast and north of HH 827 (marked in
Fig. 1) are candidate sources, however the trail of emission from HH 827 doesn't point
back to either of these. If HH 827 is driven by CW Tau then the projected length of the blueshifted outflow is 7
08 (0.29 pc).
Table 2: Angular separations, PAs and spatial extent of newly discovered HH objects in the CW Tau region.
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Figure 1:
CW Tau: mosaic of the entire CW Tau outflow. The top and middle frames
are in [SII] and the bottom frame is in H |
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Figure 2:
CW Tau: left: our [SII] image showing CW Tau and the newly
discovered HH 826 and HH 828 knots. The small white box superimposed on CW Tau marks the region shown
on the right. Right: CW Tau and the HH220 jet taken from Dougados et al. (2000). A dotted line
shows the PA of 144 |
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Figure 3:
HH 827 H |
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Figure 4:
HH 829: image of HH 829 A, B and C to the north of CW Tau in [SII] ( left) and H |
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Our [SII] images show that the redshifted HH 220 jet extends to
46
from CW Tau at a PA of 326
(Fig. 1). The jet first extends to
9
from the
source, then there is a gap of almost 20
where the jet is too faint to be seen. It becomes
visible again for a distance of
17
before terminating in the bright knot HH 826 C.
Further out a trio of knots (HH 828) are found at
4
3 from CW Tau and are only seen in
[SII] (Figs. 1 and 2). The most western knot is at a PA of
334
from CW Tau and the most eastern is at 342
.
There are three known IRAS sources in the vicinity of HH 828 (marked in Fig. 1) and it is possible that the source of the
HH 828 knots is one of these or CW Tau itself. Proper motion studies would help distinguish between
these possibilities.
There is a distance of
10
8 (0.44 pc) between HH 828 and the next HH object along this
direction, HH 829 A (Figs. 1 and 4). HH 829 A, B and C are
14
9, 16
12 and 16
8 at 348
,
351
and 353
from CW Tau respectively. The
edge of this complex is approximately 37
from the northern edge of our field of view so it is
possible that further emission is present beyond this. While HH 829 A is comparable in brightness in
both H
and [SII] emission, knots B and C are brighter in [SII] and H
respectively
(Fig. 4). IRAS 04111+2820 (slightly outside the field of view of
Fig. 1) is
1
5 at a PA of 78
from HH 829 C but is highly unlikely
to be driving this set of co-linear knots given their position with respect to this source. The
projected length of this assumed CW Tau redshifted outflow is 0.69 pc (16
8). This gives a total
projected length of the CW Tau blue - and redshifted outflows of
0.98 pc.
The variation in PA in the blueshifted outflow is 40
and is 24
in the redshifted outflow.
This change in direction gives the extended outflow an inverted "S'' shape. Similar morphologies are
seen in many large-scale outflows from less evolved low-mass sources (see
Sect. 4.1) and suggests outflow precession. The change in direction is approximately
symmetrical about CW Tau which substantiates our suggestion that both HH 827 and HH 829 may be part
of this outflow. CW Tau is surrounded by a dark cloud (Fig. 1) so the majority of the
outflow is presumably obscured by this cloud. It is interesting to note however that the more distant
objects in this outflow, HH 827 and HH 829, are found at the cloud edges.
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Figure 5:
DG Tau: a) mosaic image of the region surrounding DG Tau and DG Tau B in H |
| Open with DEXTER | |
DG Tau is a low luminosity star with
8
(Cohen & Kuhi 1979) and was one of the first
TTSs to be associated with an optical jet (HH 158), noted by Mundt & Fried (1983). HST/STIS observations
show HH 158 to be at a PA of 223
with respect to DG Tau (Bacciotti et al. 2002) and that the
blueshifted HH 158 "micro-jet'' can be traced to within
0
1 from the star
(Bacciotti et al. 2000). Larger scale studies show the HH 158 outflow to extend to
11
,
with
a number of resolved knots (Eislöffel & Mundt 1998). A redshifted jet
1
in length is detected
0
45 from the source (Lavalley et al. 1997). There is a semi-circular nebula associated
with DG Tau (Mundt et al. 1987) which HST data resolves as three nested arcs of reflection at 2
,
5
and 10
from DG Tau (Stapelfeldt et al. 1997). The axis of symmetry of all three arcs is
225
with respect to DG Tau which is well aligned with the PA of HH 158, suggesting that
these arcs are the illuminated edges of a cavity carved by the blueshifted jet.
DG Tau B is located 47
south and 28
west of DG Tau and is a low luminosity Class
I source with
= 0.88
(Jones & Cohen 1986). It is the driving source of an optical jet (HH 159)
also found by Mundt & Fried (1983) and seen to be bipolar by Jones & Cohen (1986). HST images have resolved DG Tau
B as a compact bipolar reflection nebula with no optically visible star (Stapelfeldt et al. 1997). The
eastern lobe of the reflection nebula is "V'' shaped and the PA of its axis of symmetry
is 122
(Padgett et al. 1999). The 56
redshifted jet and 15
blueshifted jet have been observed both
in imaging mode (Mundt et al. 1991; Eislöffel & Mundt 1998; Mundt & Fried 1983) and spectroscopically
(Mundt et al. 1987; Jones & Cohen 1986; Eislöffel & Mundt 1998). Position angles of 122
for the blueshifted jet
and 296
for the redshifted jet were determined by Mundt et al. (1991). However examination of our images would
suggest that the PA of the blueshifted jet is closer to 116
i.e. the two jets are diametrically
opposed as one might expect. In either case, the blueshifted jet is approximately coincident with the
axis of symmetry of the reflection nebula, suggesting that the "V'' delineates the walls of a cavity
cleared by it. The redshifted jet passes through the centre of a well collimated redshifted
CO emission
lobe (Mitchell et al. 1994,1997).
Table 3: Angular separations, PAs and spatial extent of newly discovered HH objects in the DG Tau and DG Tau B region.
The most spectacular object in this outflow is HH 702 - an
4
long shock system to
the southwest of DG Tau. This object has already been noted by Sun et al. (2003), however our H
images show more detail than the [SII] image of Sun et al. (2003). HH 702 consists of five bright knots
(Fig. 5d) (one of which (E) was not noted by Sun et al. 2003), two fainter knots (F and G)
and a trail of emission to the northeast. From our images, the trail of emission is first seen 7
9
from DG Tau at a PA of 218
,
pointing back towards DG Tau, and stretches a distance of 2
75 to Knot A. Knot A is an intense emission knot at 10
6 from DG Tau, with a star directly to the
east. Knots C and D are on either side of a star and can be seen more clearly in the continuum
subtracted image inset in Fig. 5d. While a number of IRAS sources in the vicinity have
been previously suggested as possible sources for HH 702 (Sun et al. 2003), we think it is more likely
that this object is driven by DG Tau given the alignment between HH 702 and HH 158. The most distant
optically visible object in the blueshifted outflow, Knot G of HH 702 is 12
32 from DG Tau, which
is 0.5 pc in projected length at a distance of 140 pc to the Taurus-Auriga cloud.
Our observations reveal a new HH complex (HH 830) in the DG Tau outflow, details of which are given in
Table 3. HH 830 is a faint complex 9
6 to the northeast of DG Tau and consists
of three separate emission objects A-C (Fig. 5c). HH 830 A is a 44
long
linear object orientated east/west and dips southwards towards its western edge. HH 830 B is
11
3 from DG Tau and is brighter than HH 830 A but is much smaller in size
(Fig. 5b). HH 830 C is the most distant optically visible object in this outflow and
appears to be two separate emission regions at 14
1 (at PA of 47
)
and 14
4 (at PA of
50
)
from the source (Fig. 5b). This object is at one edge of our image and
there there might be more emission further east. The HH 830 knots are comparable in H
and
[SII] emission. Both HH 830 A and the centre of HH 830 C are along a PA of
48
with
respect to DG Tau. Thus they are reasonably well aligned with the redshifted jet which we estimate to
be at 44
from the images of Lavalley et al. (1997). HH 830 B is slightly off this axis, at a PA of 52
.
The total length of the redshifted outflow is 14
4 i.e. 0.59 pc, giving the total
projected length of the DG Tau bipolar outflow to be 1.09 pc.
The outflow direction changes by 5
in the blueshifted outflow and 8
in the redshifted
outflow giving the extended outflow a "C'' shaped morphology, with DG Tau at the apex of the "C''.
Similar morphologies have been noted in a small number of large-scale outflows from less evolved
sources, for example the HH 366 outflow in Barnard 5 (Bally et al. 1996). This morphology may be analogous
to the head-tail extragalactic radio sources where a curved morphology is created between the radio
source (head) and the bipolar jet (tails) due to the motion of the source through the ISM
(Valentijn 1981; Edge & Rottgering 1995). In the YSO case, typical stellar velocities of around 5-10 km s-1
with respect to the parent cloud, combined with jet velocities of approximately 150 km s-1, might
produce a similar effect.
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Figure 6:
HH 836 and HH 837: the objects to the southeast of DG Tau B are shown here in both
H |
| Open with DEXTER | |
Our observations also reveal two faint new objects to the southeast of DG Tau B, with a third more
evident one further out in the same direction (Figs. 5 and 6),
details of which are given in Table 3. HH 836 A is at
2
6 from the
source and is seen only in H
.
HH 836 B is at 4
4 from DG Tau B and is seen in
both H
and [SII]. A trail of emission appears to curve back towards HH 836 A from HH 836 B in the H
image. These HH objects are quite faint and diffuse. The most distant optically visible
object in the blueshifted outflow is HH 837 at 10
4 from DG Tau B. In [SII] this object appears
to have a "V'' shaped morphology pointing eastwards. In H
it is much stronger and is clearly bow
shaped with some emission over-lapping the [SII] emission to the west of the bow
(Fig. 6). There is no indication of this bow shock in the [SII] emission. Both
HH 836 A and HH 837 are at a PA of 116
and 117
respectively with respect to DG Tau B
and are well aligned with the blueshifted HH 159 jet. HH 836 B is slightly off this axis at 122
suggesting that the direction of the blueshifted outflow has only varied slightly over the 10
4
distance from the source. Although IRAS 04244+2557 is a possible driving source for some of these
HH objects (see Fig. 5) it seems more than coincidental that all three are aligned with the
DG Tau B jet. The length of this outflow from the redshifted HH 159 jet to HH 837 is 11
3 which
is a projected length of 0.46 pc. It is interesting to note that the opening angle for the blueshifted
jet was initially estimated to be
17
i.e. almost four times that of the redshifted jet at
4.5
(Mundt et al. 1991). Our images of the extended blueshifted outflow show that it has
clearly recollimated; the extended opening angle (to HH 837) is now 3
.
Two other HH objects are found in this region which do not appear to be related to either the DG Tau
or the DG Tau B outflows. HH 838 is 1
6 at a PA of 286
from DG Tau B and is a faint,
43
by
4
linear HH object running north/south (Fig. 5) seen
only in H
emission. All known IRAS sources in the regions are marked in Fig. 5
but none of these appear to be a likely driving source for HH 838. Our images do not show any other HH
emission aligned with HH 838. The second HH object, HH 839 to the east of DG Tau B, consists of three
"knots'' (seen clearly in Fig. 5e), of which the most northwestern one appears to be a
mixture of continuum and HH emission and is probably the location of the source driving the outflow.
The other two knots which are at a PA of 126
with respect to this assumed source appear to be
an
10
long outflow and are equally strong in H
and [SII]. This outflow is
approximately parallel to the DG Tau B outflow. HH 839 is quite bright in our I band images so it
possibly contains some reflection nebulosity as well. We can find no other obvious driving source for
this outflow.
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Figure 7:
DO Tau/HV Tau: a) mosaic of the DO Tau and HV Tau C regions showing the newly
discovered HH objects HH 831-HH 834. The positions of candidate sources for these HH objects are
marked. HH 230 is not seen in our optical images because of the DO Tau nebulosity, however the dashed
line from DO Tau is at 70 |
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DO Tau is a CTTS associated with an arc-like nebula. A bipolar jet (HH 230) extending for
approximately 2
to 4
was observed spectroscopically from DO Tau by Hirth et al. (1994)
with the redshifted jet at a PA of
70
(Hirth et al. 1994). DO Tau is an M0 star
(Herbig & Bell 1988) with a mass in the range 0.3-0.7
and an age of about
years
(Hartigan et al. 1995; Beckwith et al. 1990). To the east of DO Tau is the triple system HV Tau consisting of a close
binary, A and B (Simon et al. 1996), and a third component C
4
northeast of the close binary.
HV Tau C is an actively accreting CTTS (Woitas & Leinert 1998) and a bipolar "micro-jet''
1
5
in length has recently been observed emerging from it (Stapelfeldt et al. 2003). We have estimated the PA
of its blueshifted jet to be at 25
with respect to the source from the images of
Stapelfeldt et al. (2003).
Five HH objects were found in this region and are marked in Fig. 7a with details given
in Table 4. Neither the DO Tau nor the HV Tau C jets are seen in our optical
images because of the bright nebulosity around both stars. HH 831 is found roughly northeast of
DO Tau
and is seen in both [SII] and H
although there are morphological differences between these two
images. HH 832 and HH 833 are also seen to the northeast of DO Tau however they are only visible in [SII]. HH 834 is the only object to the southeast and is seen only in H
.
In H
images (Fig. 9) HH 831 A is a 52
long structure consisting of
three small joined arcs and is fainter towards the northwest and HH 831 B is a diffuse knot.
In [SII]
images (Fig. 8) HH 831 A is seen as two separate emission regions, the most
distant of which is at 10
8 from DO Tau. HH 831 B contains a number of bright emission regions
in [SII], more than are seen in H
and is at a distance of 11' from DO Tau. HH 831 B is only
36
from the eastern edge of our field of view so it is very possible that there is more
emission in this direction. HH 831 is at a PA of
74
with respect to DO Tau and is well
aligned with the redshifted jet.
HH 832 (Fig. 8) is seen only in [SII] and is at 78
and 7
7 from DO
Tau. It is an
6
long linear object with faint emission to the northeast. There is a
nearby trail from a passing satellite.
HH 833 (Fig. 7a) is a diffuse region 4
6 from HV Tau C at a PA of 25
and
is seen only in [SII]. HH 705, to the north of HH 831, is a complex object containing a number of
bright emission regions (Figs. 7b and 7c). This object was discovered by Sun et al. (2003)
however our images show it to be more intense and complex than their [SII] images. This object may be a
bow shock, with faint emission trailing to the southeast and southwest forming the wings and there is a
1
3 long trail to the south. Its total width, as measured between the edges of the wings, is
1' and its total length is 1
9. HH 834 is very faint and seen only in H
(Fig. 7d). It is linear and has a total length of 42
.
Table 4: Angular separations, PAs and spatial extent of newly discovered HH objects in the DO Tau and HV Tau C region.
The locations of these new objects in relation to previously known outflows suggests possible links.
HH 230 is at
70
with respect to DO Tau so it is likely that HH 831 at 74
,
and
possibly HH 832 at a PA of 78
,
are part of the same outflow. There is a gap of
7
7
(0.43 pc) between the 4
redshifted HH 230 jet and HH 832 where no HH emission is seen. If
HH 831 and HH 832 are driven by DO Tau then the length of the redshifted outflow is
11
07
(0.45 pc).
Considering its alignment with the previously known "micro-jet'' from HV Tau C, it is most likely
that HH 833 is driven by this source. HH 705 could also be part of this outflow. Both the blueshifted
jet from HV Tau C and HH 833 are at 25
with respect to HV Tau C whilst HH 705 is at
36
with respect to this source at a distance of 12
from it. HH 705 is
7
7
from HH 833 and it is possible that the outflow direction could have changed by 11
over this
distance. The southern trail of emission from HH 705 might suggest that its driving source is situated
to its south rather than southwest. In this case the radio sources LDN 1527 1 or LDN 1527 2 in
LDN 1527 (Anglada et al. 1992) are possible driving sources (as suggested by Sun et al. (2003), however it is
unlikely that LDN 1527 1 could generate such a large object so nearby. We think HV Tau C is the most
likely source of this object. Assuming HH 833 and HH 705 are driven by HV Tau C, the projected length
of this outflow is 0.49 pc (12
). At present there is no obvious driving source for HH 834.
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Figure 8:
HH 831 and HH 832 [SII]: [SII] image of the newly discovered objects HH 831 and
HH 832. Note that the morphology of HH 831 is quite different here to the H |
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Figure 9:
HH 831 H |
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Figure 10:
RW Aur H |
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The blueshifted component of the HH 229 bipolar jet is at a PA of
130
with respect to
RW Aur A (Dougados et al. 2000; Hirth et al. 1997; Mundt & Eislöffel 1998). [SII] images of Mundt & Eislöffel (1998) show the redshifted and
blueshifted outflows to have lengths of 50
and 106
respectively, implying a total
projected length of
0.1 pc at a distance of 140 pc. Both sides are well collimated, with a full
opening angle for the redshifted jet of less than 6
(Woitas et al. 2002). The detection of emission in
the redshifted jet can be traced back to 0
1 from the source which implies an upper limit of
15 AU
for the projected radius of its circumstellar disk.
Table 5: Angular separations, PAs and spatial extent of the newly discovered HH object in the RW Aur outflow.
Our images reveal a large object (HH 835) 5
37 to the northwest of RW Aur (See
Fig. 10 and Table 5). We suggest that this object is a bow shock with
only the
30
long northern wing visible in our H
images (Fig. 11).
Given the position of HH 835 on the known axis of the RW Aur outflow (PA of 310
with respect
to RW Aur) we suggest that this object is part of the redshifted RW Aur A outflow. There is a distance
of
4
6 between the end of the redshifted jet and HH 835 in which there is no optical
evidence for outflow activity. The total observed projected length of the RW Aur outflow from the
blueshifted jet to HH 835 is 0.29 pc (7').
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Figure 11:
HH 835 H |
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Table 6: Outflow lengths, dynamical timescales and degree of collimation for the five newly discovered parsec-scale outflows from (Class II) CTTSs and for the serendipitously discovered outflow from the Class I source DG Tau B.
We have shown that five of the seven CTTSs examined in the Taurus-Auriga Cloud (namely CW Tau, DG Tau, DO Tau, HV Tau C and RW Aur) drive outflows of the order of 1 pc in length. We have estimated the length, dynamical timescale and degree of collimation for all six of the outflows discussed in Sect. 3 and these are presented in Table 6. Here we examine the parameters and the morphological trends of these CTTS outflows in more detail, and compare them to large-scale outflows from more embedded Class I sources. These trends can be used to infer details about the source, the propagation of the outflow into the ambient medium, and the evolution of the outflows with time.
Typically many large-scale outflows from Class I sources are either "S'' shaped with the driving source approximately in the middle of the "S'' - for example the HH 47 outflow (Heathcote et al. 1996), HH 34 outflow (Bally & Devine 1994) and the PV Cephei outflow (Reipurth et al. 1997) to name but a few; or the rarer "C'' shaped with the source at the apex of the "C'' - for example the HH 366 outflow in Barnard 5 (Bally et al. 1996). It can be seen from the images presented in Sect. 3 that many of the outflows from CTTSs show evidence for some variations in PA with time, the effect being most evident in the CW Tau outflow. This outflow delineates an inverted "S'' shape centered on CW Tau with the northern part of the "S'' more elongated than the southern part. The change in outflow direction is possibly due to precession of the outflow axis (Masciadri & Raga 2002; Raga et al. 2001).
It has also been noted from large-scale outflows driven by less evolved sources that the size and complexity of the HH shocks increases with distance from the source. As the supersonic outflow propagates through the parent cloud it interacts with both the ambient medium and slower, previous ejecta producing the HH shocks observed. Many of these shocks fade quickly with time, it is only the strongest and largest shocks that remain. As a consequence of this, the gap between consecutive HH objects/complexes increases with distance as the majority of the more distant shocks quickly fade leaving just a few, larger shocks (Bally & Devine 1997; Reipurth & Bally 2001). As these extended shocks have undergone many interactions with their surroundings, and have had time to evolve, they will often be complex, chaotic objects rather than the simple knot-like structures seen closer to the young star. Most of the outflows from CTTSs presented here also demonstrate these trends.
The field of view captured by the Wide Field Camera is
34
square which projects to a
maximum detectable outflow length of 1.4 pc at the distance of the Taurus-Auriga Cloud. Outflow
morphology suggests that the distance between consecutive HH objects complexes increases exponentially
with distance from the source (Sect. 4.1) so if there is emission beyond our field of
view then it may easily be on scales of tens of parsecs, near the edges of the Taurus-Auriga Cloud
boundaries, and well beyond the field of view of the WFC.
The apparent dynamical timescales for these outflows is estimated in Table 6, assuming the most distant objects are moving at a velocity of 50 km s-1. Values of around 104 years are derived thus we are only observing a fraction of the stars' outflow histories.
Our observations suggest that, in all cases, the outflows have blown out of the associated clump. Many of the most distant objects in the outflows are at the clump edges while a few, most notably HH 830 and HH 702 in DG Tau are clearly well beyond. There is little doubt based on statistically estimated lifetimes that these outflows are even larger than our field of view, and thus our data supports the idea that they have blown out of their parent cloud. Large-scale outflows blowing out of their parent cloud is also a well documented occurrence in outflows from Class I low-mass sources, as our own observations of DG Tau B show. We have previously shown that this also occurs for outflows from intermediate-mass YSOs (McGroarty et al. 2004).
The morphology and location of the HH objects/complexes associated with the five CTTSs suggest long quiescent outflow phases punctuated by mass ejections of varying strength. According to this scenario, the most violent of the latter have given rise to the most distant (from the YSO), long-lasting and extended HH complexes that we see today. Reipurth & Aspin (1997, and references therein) have suggested that these major ejection events occur when the parent star undergoes FU Orionis-type outbursts, or FUor events. Before addressing whether this is the case, and explaining why we think our sample, albeit small, lends considerable weight to the hypothesis, it is worthwhile saying a few words about the FU Orionis phenomenon.
When a YSO undergoes an FUor outburst, its optical brightness increases by several orders of magnitude before decaying back to the pre-outburst luminosity over 50-100 years (Hartmann & Kenyon 1996). The spectra of these so-called FUors in quiescence is that of a CTTS (Hartmann & Kenyon 1996), and there are at least nine known FUors (Hartmann & Kenyon 1996) including the prototypical source - FU Orionis itself (Herbig 1977). Almost immediately after their discovery it was suggested that FUor events could give rise to Herbig-Haro outflows (Reipurth 1985; Dopita 1978). More recently, as already stated, Reipurth & Aspin (1997) investigated this possible connection, basing their conclusions largely on a sample of embedded Class I sources. As it is accepted that in quiescence FUors are CTTSs it seems more appropriate to examine outflows of the latter for any "fossil record'' of FU Orionis-type outbursts. In particular it is not obvious a priori that the outburst timescales for Class I and Class II stars are similar.
Examining Table 6 we see that the dynamical timescales of the extended HH complexes, associated with our CTTSs, are typically 104 years. Herbig (1977) and Herbig et al. (2003) have estimated the mean time between successive FUor outbursts is 104 years, suggesting a clear link. Moreover the relative number of FUors in comparison to CTTSs also supports this link.
The morphological trends observed in the CTTSs outflows are comparable to those noted in younger sources i.e. increasing distance between successive HH objects coupled with increased size and complexity with distance from the source. In a few cases, small variations in the direction of propagation of the outflow have been found. The high degree of collimation of the five extended outflows from CTTSs compared well with that observed in the case of extended large-scale outflows from less evolved sources, suggesting that outflows remain focussed even as the source evolves from the Class I to the Class II stage. It is clear that the observed parsec-scale lengths of the CTTS outflows are minimum values and in reality they are much larger. These outflows all show evidence for having blown out of the parent cloud.
The apparent dynamical timescale of these extended outflows is typically a few times 104 years. This suggests a linkage between the major accretion events that give rise to the largest HH complexes and the FU Orionis phenomenon. As FU Orionis stars are CTTSs in quiescence, the extended outflows of the latter provide the best "fossil record'' to test this linkage.
Acknowledgements
We thank the anonymous referee for helpful comments that clarified the presentation of these results. F.McG. and T.P.R. acknowledge support from Enterprise Ireland. This research has made use of the SIMBAD database, operated at CDS, Strasbourg, France.