Exposure | PA [![]() |
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YLW 16 A (p - I) | 178 | 1.7 | 19 | 97 | - | 3 | 0.0074 |
YLW 16 A (p - II) | 178 | 2.5 | 27 | >99 | <1 | <1 | 0.020 |
YLW 16 A (o) | 88 | 2.2 | 24 | 70 | 1.7 | 28 | 0.078
|
YLW 16 A (o) - 1 | 88 | 2.0 | 22 | 32 | 1.1 | 67 | 0.011 |
YLW 16 A (o) - 2 | 88 | 1.9 | 20 | 31 | 1.4 | 68 | 0.0046 |
YLW 16 A (o) - 3 | 88 | 1.7 | 19 | 93 | 1.0 | 5.7 | 0.0042 |
YLW 16 A (o) - 4 | 88 | 1.8 | 20 | 78 | 10 | 12 | 0.010 |
YLW 16 A (o) - 5 | 88 | 1.7 | 19 | 87 | 4.9 | 7.8 | 0.0079 |
YLW 16 A (o) - 6 | 88 | 2.0 | 22 | 84 | 7.6 | 8.2 | 0.0042 |
YLW 16 A (o) - 7 | 88 | 2.0 | 22 | 4.5 | 3.2 | 92 | 0.0087 |
Notes. The position
angles (PA) of the spectroscopic slit,
measured from North to East, are additionally listed. The
regions 1 to 7 represent spectra that originate in source regions with widths of
,
,
,
,
,
,
and
.
The spectra 3-5 originate closer to the
photocenter than the spectra 1, 2, 6, and 7. In contrast,
for the first three exposures listed, the counting rates within
of the spatial dimension are summarized. The quantities
and
represent the column density of water ice particles and the visual extinction derived along the line of sight (Eqs. (4), and (5)).
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