New thermal anomalies in the subsurface of Enceladus ’ South Polar Terrain 3 4
暂无分享,去创建一个
C. Sotin | R. Kirk | R. Lorenz | A. Lucas | C. Leyrat | O. Bourgeois | M. Janssen | F. Paganelli | G. Tobie | C. Howett | A. L. Gall | G. Choblet | M. Masse | R. West | A. Stolzenbach | A. Hayes | G. Veyssière
[1] C. Sotin,et al. The temperature and width of an active fissure on Enceladus measured with Cassini VIMS during the 14 April 2012 South Pole flyover , 2013 .
[2] P. Paillou,et al. Microwave dielectric constant of Titan‐relevant materials , 2008 .
[3] Irwin I. Shapiro,et al. Planetary radar astronomy , 1968, IEEE Spectrum.
[4] Rosaly M. C. Lopes,et al. Titan’s surface at 2.18-cm wavelength imaged by the Cassini RADAR radiometer: Results and interpretations through the first ten years of observation , 2016 .
[5] D. Campbell,et al. Icy Galilean Satellites: Modeling Radar Reflectivities as a Coherent Backscatter Effect , 2001 .
[6] R. A. Hanel,et al. Albedo, internal heat flux, and energy balance of Saturn , 1983 .
[7] M. Janssen,et al. Anomalous radar backscatter from Titan’s surface? , 2011 .
[8] Rosaly M. C. Lopes,et al. Cassini RADAR observations of Enceladus, Tethys, Dione, Rhea, Iapetus, Hyperion, and Phoebe , 2006 .
[9] Gabriel Tobie,et al. Enceladus's internal ocean and ice shell constrained from Cassini gravity, shape, and libration data , 2016 .
[10] C. Werner,et al. Cassini Titan Radar Mapper , 1991, Proc. IEEE.
[11] D. Matson,et al. Solid-state greenhouse and their implications for icy satellites , 1989 .
[12] R. Lorenz,et al. Probing Pluto’s underworld: Ice temperatures from microwave radiometry decoupled from surface conditions , 2016 .
[13] Richard K. Moore,et al. Microwave Remote Sensing, Active and Passive , 1982 .
[14] R. Pappalardo,et al. Structural mapping of Enceladus and implications for formation of tectonized regions , 2015 .
[15] J. L. Chute,et al. Apollo 15 measurement of lunar surface brightness temperatures thermal conductivity of the upper 1 1/2 meters of regolith , 1973 .
[16] W. Peake. Interaction of electromagnetic waves with some natural surfaces , 1959 .
[17] J. Pearl,et al. High heat flow from Enceladus' south polar region measured using 10–600 cm−1 Cassini/CIRS data , 2011 .
[18] J. Spencer. A rough-surface thermophysical model for airless planets , 1990 .
[19] M. Janssen,et al. A large-scale anomaly in Enceladus’ microwave emission , 2015 .
[20] R. West,et al. Iapetus’ near surface thermal emission modeled and constrained using Cassini RADAR Radiometer microwave observations , 2014 .
[21] C. H. Acton,et al. Ancillary data services of NASA's Navigation and Ancillary Information Facility , 1996 .
[22] Rosaly M. C. Lopes,et al. Mountains on Titan observed by Cassini Radar , 2006 .
[23] T. Owen,et al. Exploring The Saturn System In The Thermal Infrared: The Composite Infrared Spectrometer , 2004 .
[24] R. Jaumann,et al. Composition and Physical Properties of Enceladus' Surface , 2006, Science.
[25] S. W. Asmar,et al. The Gravity Field and Interior Structure of Enceladus , 2014, Science.
[26] J. A. Burns,et al. Enceladus's measured physical libration requires a global subsurface ocean , 2015, 1509.07555.
[27] T. White,et al. Lunar polarization studies at 3.1mm wavelength , 1973 .
[28] Bruce Hapke,et al. Coherent backscatter and the radar characteristics of outer planet satellites , 1990 .
[29] J. Klinger. Influence of a Phase Transition of Ice on the Heat and Mass Balance of Comets , 1980, Science.