The major portion of the molecular gas is within a velocity range of
-10 to 10 km s-1, and there are several pieces of small isolated
clouds scattered on the small scale, especially in the region of (l,
b) = () (see
Figs. 3 and 4). However, it is also found that some portion of the
CO emission shows more than one peak; many spectra show evidence that two
or more clouds are blended together in some directions, mostly from
to
(see Sect. 5).
To effectively identify these clouds from the 3-dimensional data cube
set (l, b, v), we used a code developed by Lee et al. (1997), which
is working as a user task within IRAF. Using the 12CO cube data,
they define a cloud to be an object composed of all pixels in
longitude, latitude, and velocity that are simply connected and that
lie above some threshold temperature. This is the same method
employed by Scoville et al. (1987) and Lee et al. (1990).
Ideally, one would like to define clouds with a 0 K threshold
temperature. However, low threshold temperatures are impractical in
view of the noise level in the spectra and more importantly because of
the blending of adjacent clouds which occurs in the observed region.
On the other hand, with too high a threshold temperature, regions are
severely truncated, and it is impossible to obtain a reliable estimate
of the sizes and thus the masses of the clouds. To define clouds we
should choose a reasonable threshold temperature. Above the arbitrary
threshold temperature, only those clouds with 2 or more pixels in each
l, b, and v are retained. In this way, we identify 30
clouds with a threshold temperature of 1.25 K (). One of
those is found to be very large, and seems to be blended with several
adjacent clouds with similar velocities. Using a higher threshold
temperature of 2.5 K (
) we have separated the object into
several subclouds. The number of subclouds determined in this way is
12, and the identified clouds and subclouds are listed in Table 1.
Intriguingly, the subclouds appear in two distinct mean velocity
groups, one with
1 km s-1, and the other with
km s-1, which also implies that the largest
cloud (No. 18) is a blended one. The first column is the cloud
number; centroid positions and their dispersions are given Cols. 2-5. Column 6 is
the centroid velocity and Col. 7 is the linewidth at half maximum. Peak temperature
and the number of pixels retained within the cloud follow in Cols. 8 and 9. In this
table we do not include detailed physical parameters, as distances are yet
to be determined, though the distance of cloud No. 8 was found to be
4.7 kpc, which is associated with the HII region Sh 241 (Moffat
et al. 1979).
Recently, Kawamura et al. (1998) listed the clouds in this
region using their 13CO survey conducted with
the
4-m telescope in Nagoya University. The number of clouds
identified in their survey was 7, much smaller than the number of
clouds identified in this work. The Kawamura et al. (1998)'s distance
determination toward these clouds (d=1.1 kpc) was based on
Racine (1968)'s photometry of a star BD . However,
the coordinate of the star (l,b) = (
) is
very close to the HII region Sh 241, the distance of which is
known to be 4.7 kpc (Moffat et al. 1979), which is by far more distant
than those of the presumably local clouds. Thus, the distances of the
clouds with noticeable opaqueness are likely ill-determined and should
be redetermined. In fact, we are imaging these regions with deep CCD
observations to estimate the distances, and for further analysis. The
physical properties of the identified clouds will be presented in a
separate paper with determination of distances of the clouds (Lee et al. in
preparation).
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Figure 5: Average of all 7 000 spectra. While there is sharp cut in the positive-velocity emission regime at 7 km s-1, there is more extended emission in a negative-velocity regime up to -25 km s-1 |
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Figure 6: Global integrated position-velocity map. The lowest contour is 4.5, 9, and 15 K, and the increment between the levels above 15 K is 6 K. The grey scale range is 2 to 60 K |
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