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70 m | 100 m | 160 m | 250 m | 350 m | 500 m | |
Published | 1071 | 1052 | 1012 | 763 | 493 | 423, 704 |
22 | 21 | 20 | 16 | 10 | 8, 16 | |
Herschel | 169 | 192 | 166 | 168 | 92 | 52 |
17 | 19 | 17 | 17 | 10 | 7 | |
Nonthermal | 6.3 | 8.1 | 11.2 | 15.4 | 19.4 | 24.9 |
0.6 | 0.7 | 0.9 | 1.1 | 1.3 | 1.6 | |
Warm dust | 120 | 63 | 22 | 7.0 | 3.1 | 1.2 |
12 | 6 | 2 | 0.8 | 0.4 | 0.2 | |
Cold IS dust | 18 | 76 | 123 | 141 | 69 | 27.5 |
4 | 11 | 17 | 17 | 10 | 7 | |
Cool dust | 25 | 295 | 10 | 4.6 | 0.5 | -1.6 |
7 | 11 | 17 | 17 | 10 | 4 |
Notes. (1) MIPS (Hines et al. 2004); (2) AKARI 90 and 170 m (Sibthorpe et al. 2010); (3) BLAST 250, 350 and 500 m (Sibthorpe et al. 2010); (4) SCUBA 450 m (Dunne et al. 2003); (5) after subtracting a line contribution of 16 Jy (see Sect. 3).
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