Dust in the polar region as a major contributor to the IR emission of AGN
Sebastian F. Hoenig (1), Makoto Kishimoto (2), Konrad R. W. Tristram, (2), M. Almudena Prieto (3), Poshak Gandhi (4,5), Daniel Asmus (2), Robert, Antonucci (1), Leonard Burtscher (6), Wolfgang J. Duschl (7,8), Gerd Weigelt, (2) ((1) UCSB, (2) MPIfR, (3) IAC, (4) ISAS, JAXA

TL;DR
This study uses interferometry to show that most mid-IR emission in NGC 3783's AGN comes from a polar dusty wind rather than the traditional torus, challenging existing models.
Contribution
It provides high-resolution evidence that mid-IR emission in AGN is dominated by polar dust, not the torus, suggesting a need to revise current AGN IR emission models.
Findings
Mid-IR emission is elongated toward the polar axis, not the equatorial plane.
Half-light radii at 12.5 μm are approximately 4.2 pc by 1.4 pc.
Majority of mid-IR emission (60-90%) is from polar-elongated dust.
Abstract
(abridged) It is generally assumed that the distribution of dust on parsec scales forms a geometrically- and optically-thick entity in the equatorial plane around the accretion disk and broad-line region - dubbed "dust torus" - that emits the bulk of the sub-arcsecond-scale IR emission and gives rise to orientation-dependent obscuration. Here we report detailed interferometry observations of the unobscured (type 1) AGN in NGC 3783 that allow us to constrain the size, elongation, and direction of the mid-IR emission with high accuracy. The mid-IR emission is characterized by a strong elongation toward position angle PA -52 deg, closely aligned with the polar axis (PA -45 deg). We determine half-light radii along the major and minor axes at 12.5 {\mu}m of (4.23 +/- 0.63) pc x (1.42 +/- 0.21) pc, which corresponds to intrinsically-scaled sizes of (69.4 +/- 10.8) rin x (23.3 +/- 3.5) rin…
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