Keck and VLT AO observations and models of the uranian rings during the 2007 ring plane crossings

• Published in: Icarus (New York, N.Y. 1962) N.Y. 1962), 2013-11, Vol.226 (2), p.1399-1424
• Main Authors: de Pater, Imke, Dunn, David E., Stam, Daphne M., Showalter, Mark R., Hammel, Heidi B., Min, Michiel, Hartung, Markus, Gibbard, Seran G., van Dam, Marcos A., Matthews, Keith
• Format: Article
• Language: English
• Subjects: Angles (geometry); Density; Dust; Infrared observations; Mathematical models; Monte Carlo methods; Planes; Planetary rings; Planets; Uranus; Very Large Telescope
• ISSN: 0019-1035; 1090-2643
• DOI: 10.1016/j.icarus.2013.08.001

•We see a pronounced opposition effect in the ∊ ring.•A 140km thick sheet of dust extends from the λ ring to the planet.•The ζ ring has a full vertical extent of 860km.•The ζ ring has a pronounced density enhancement in the mid-plane.•The ηc ring is optically thin and less than several tens of km in the vertical direction. We present observations of the uranian ring system at a wavelength of 2.2μm, taken between 2003 and 2008 with NIRC2 on the W.M. Keck telescope in Hawaii, and on 15–17 August 2007 with NaCo on the Very Large Telescope (VLT) in Chile. Of particular interest are the data taken around the time of the uranian ring plane crossing with Earth on 16 August 2007, and with the Sun (equinox) on 7 December 2007. We model the data at the different viewing aspects with a Monte Carlo model to determine: (1) the normal optical depth τ0, the location, and the radial extent of the main rings, and (2) the parameter Aτ0 (A is the particle geometric albedo), the location, and the radial plus vertical extent of the dusty rings. Our main conclusions are: (i) The brightness of the ∊ ring is significantly enhanced at small phase and ring inclination angles; we suggest this extreme opposition effect to probably be dominated by a reduction in interparticle shadowing. (ii) A broad sheet of dust particles extends inwards from the λ ring almost to the planet itself. This dust sheet has a vertical extent of ∼140km, and Aτ0=2.2×10−6. (iii) The dusty rings between ring 4 and the α ring and between the α and β rings are vertically extended with a thickness of ∼300km. (iv) The ζ ring extends from ∼41,350km almost all the way inwards to the planet. The main ζ ring, centered at ∼39,500km from the planet, is characterized by Aτ0=3.7×10−6; this parameter decreases closer to the planet. The ζ ring has a full vertical extent of order 800–900km, with a pronounced density enhancement in the mid-plane. (v) The ηc ring is optically thin and less than several tens of km in the vertical direction. This ring may be composed of macroscopic material, surrounded by clumps of dust.