The Rosette Molecular cloud is a star-forming region of gas
and dust in the Milky Way which exhibits a highly complex structure
with regions of varying density and temperature. The purpose
of studying the Rosette nebula was to attempt to better understand
the process of star formation. Infrared observations show that
stars are forming in the cloud, and much is known about how
stars form (through the collapse of gravitationally bound matter).
The initial mass function of stars, that is, the number of
stars that form at a given mass, is also well-determined. However,
the processes connecting the conditions in a molecular cloud
to the observed properties of young stars are not well understood.
We would like to know more about the conditions which make
star formation favorable, for example, how massive star-forming
regions must be, whether we can observe star formation being
influenced by temperature, density perturbations, etc. We want
to know why some regions form stars while others don't. We
would also like to be able to connect conditions in molecular
clouds with the observed properties of young stars, especially
the initial mass function.
Our data consisted of two maps of
the region, one a 3-D data cube mapping emission from the 13CO
molecule in position and velocity space, and one a 2-D map
of
12CO emission over the surface of the cloud. Each
data set consisted of 50,000 spectra at a resolution of 50" (0.3
pc) and extended over 3 degrees (60 pc). The two data sets
were complementary, since the emission line of the 1 —> 0
rotational transition of the 13CO molecule is optically
thin, which allows us to trace the location of mass in the
cloud, and the 12CO emission line is optically thick,
which gives a measurement of surface temperature. These pieces
of information, when combined, allowed us to determine the
masses of various regions in the cloud. We approached this
study of the Rosette molecular cloud by dividing the nebula
into discrete clumps of emission and studying the physical
properties of these clumps, including their size, mass, linewidth,
temperature, and other quantities associated with the clump
like aspect ratio, degree of virialization, and distance from
the HII region (an area of violent star formation activity
in the cloud). We then looked for and investigated various
trends in the data, and studied the effects of smoothing the
map over various ranges to better understand how the cloud
is structured over different size scales and how the resolution
of observations affects the results obtained. We also located
IRAS point sources within the cloud whose colors matched those
of regions of recent star formation in an attempt to better
understand why the regions associated with these sources should
be more likely to form stars.
12CO peak temperature map of the Rosette molecular cloud. The
cross marks the center of the Rosette nebula and the molecular gas forms a
large ring around this. Embedded star forming regions within the cloud,
detected at infrared wavelengths are shown by the stars. We studied the
structure in the cloud at different scales and the properties of the star
forming regions.
Several interesting trends emerged from our analysis of the
clumps of material in the Rosette nebula. Density remained
roughly constant with the size of the clump, for example, which
was also true at all scales of the data. The size-linewidth
relation, a well-studied trend in molecular clouds that displays
the degree to which the kinematics of the cloud are interconnected
on various scales, exhibited a large degree of scatter and a different
power law than that generally measured for molecular clouds . This power
law relationship remained constant over all scales of the nebula. The influence
of the HII region was evident in the temperature of the clumps, but seemed
to have little effect on other aspects of the cloud. There was a slight
trend for objects near the HII region to be smaller and more dense, which
is consistent with expectations for the effects of an expanding bubble
of gas, but there was no detectable effect on degree of virialization,
which would tend to promote or inhibit star formation. Alpha, the virialization
parameter, scaled approximately as M-2/3 over all size scales of the cloud,
which is consistent with predictions made by Bertoldi and McKee (1992)
for pressure-confined clumps. There was a tendency for the measured alpha
to increase with smoothing scale, indicating that size scales are important
for virialization. This was supported by the investigation of clumps associated
with IRAS sources: those clumps tended to be towards the high-mass, low-alpha
end of the spectrum, although most still had α > 1. This indicates
that they are gravitationally unbound, contrary to expectations for a star-forming
region. This, along with the fact that our 13CO observations,
sensitive to large-scale properties of the cloud, are unable to reveal
differences between these regions, suggests that perhaps the ranges over
which differences in star forming and non-star forming regions occur are
at smaller scales than 50" (0.3 pc), the resolution of our data. Other
than the trend for alpha to increase with smoothing, however, the cloud
was remarkably self-similar over a range of size scales, indicating the
presence of fractal structure.