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Figure 1:
L-packet injection into the core: the packet is injected
from a random point (![]() ![]() ![]() ![]() |
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Figure 2:
Density distribution on the x=0 plane a) for a flattened
asymmetric core with equatorial-to-polar optical depth ratio e=1.5
and p=4 (model 1.1), b) for a more flattened asymmetric core, with
e=2.5 and p=4 (model 1.2), c) for a core with e=1.5 and p=1
(model 1.3), and d) for a more flattened core, with e=2.5 and p=1
(model 1.4). We plot iso-density contours every
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Figure 3: Temperature distribution on the x=0 plane, for the models presented in Fig. 2. We plot iso-temperature contours from 8 to 18 K, every 2 K. |
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Figure 4: SED for the core models in Figs. 2 and 3; model 1.1 (e=1.5, p=4; short-dashed line), model 1.2 (e=2.5, p=4; solid line), model 1.3 (e=1.5, p=1; dash-dot line) and model 1.4 (e=2.5, p=1; long-dashed line). The SED of each core is independent of the observer's viewing angle. The dotted line on the graph corresponds to the incident/background SED. |
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Figure 5:
A perpendicular cut through the centre of the core images
presented in Fig. 7 for model 1.2 at 200
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Figure 6:
Isophotal maps at 200
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Figure 7: Same as Fig. 6, but for a more flattened core, with equatorial-to-polar optical depth ratio e=2.5 and p=4 (model 1.2). |
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Figure 8: Same as Fig. 6, but for a core with equatorial-to-polar optical depth ratio e=1.5 and p=1 (model 1.3). |
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Figure 9: Same as Fig. 6, but for a core with equatorial-to-polar optical depth ratio e=2.5 and p=1 (model 1.4). |
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Figure 10:
Isophotal maps at 850
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Figure 11: Same as Fig. 10, but for a more flattened core, with equatorial-to-polar optical depth ratio e=2.5 and p=4 (model 1.2). |
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Figure 12: Same as Fig. 10, but for a core with equatorial-to-polar optical depth ratio e=1.5 and p=1 (model 1.3). |
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Figure 13: Same as Fig. 10, but for a core with equatorial-to-polar optical depth ratio e=2.5 and p=1 (model 1.4). |
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Figure 14:
The effect of the parent cloud on cores. Temperature profiles
of a non-embedded core (model 1.2; dashed lines), and of a core at the
centre of an ambient cloud with visual extinction
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Figure 15:
Temperature distribution on the x=0 plane, for the same model presented in Figs. 2b and 3b
(e=2.5, p=4, model 1.2), but embedded in the centre of an ambient
molecular cloud with visual extinction
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Figure 16:
Same as Fig. 5, i.e. model 1.2, but for a
core embedded in a uniform molecular ambient cloud with visual extinction
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Figure 17:
Same as Fig. 5, i.e. model 1.2, but for a
core embedded in a uniform molecular ambient cloud with visual extinction
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Figure 18:
The effect of an UV-enhanced ISRF on embedded cores. Temperature
profiles of a core with the same set of parameters as model 1.2 (p=4,
e=2.5), embedded in a uniform density ambient cloud with visual extinction
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Figure 19:
Density distribution on the x=0 plane for a core with
axial asymmetry, south-to-north pole optical depth ratio e=2.5
and p=4 (model 2.2). We plot iso-density contours every
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Figure 20: Temperature distribution on the x=0 plane, for the model presented in Fig. 19 (e=2.5, p=4, model 2.2). We plot iso-temperature contours from 8 to 18 K, every 2 K. The denser, southern parts of the core are colder. |
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Figure 21:
Isophotal maps at 200
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Figure 22:
Isophotal maps at 850
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