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Enceladus' Damascus Sulci

Dr Carly Howett

Associate Professor of Space Instrumentation

Research theme

  • Exoplanets and planetary physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Planetary surfaces
  • Solar system
  • Space instrumentation
carly.howett@physics.ox.ac.uk
Atmospheric Physics Clarendon Laboratory, room 314
  • About
  • Publications

Surface Compositions of Trojan Asteroids

Space Science Reviews Springer 220:3 (2024) 28

Authors:

Joshua P Emery, Richard P Binzel, Daniel T Britt, Michael E Brown, Carly JA Howett, Audrey C Martin, Mario D Melita, Ana Carolina Souza-Feliciano, Ian Wong

Abstract:

The Jupiter Trojan asteroids are a key population for understanding the chemical and dynamical evolution of the Solar System. Surface compositions of Trojans, in turn, provide crucial information for reconstructing their histories. NASA’s Lucy mission will soon complete the first spacecraft reconnaissance of this population. This review summarizes the current state of knowledge of Trojan surface compositions and looks ahead to expected advances in that knowledge from Lucy. Surface compositions of Trojans remain uncertain due to a relative lack of diagnostic absorption features, though dedicated observations have begun to provide some clues to compositions. Trojans have uniformly low albedos, with a population average of ∼5.3%, and red spectral slopes at ultraviolet, visible, and near-infrared wavelengths. A bimodality of spectral slopes has been detected and confirmed across all these wavelengths, and the ratio of “less-red” to “red” Trojans increases with decreasing size. A broad absorption at ∼3.1 μm in some less-red Trojans may indicate the presence of N-H bearing material. Mid-infrared emissivity spectra reveal the presence of fine-grained anhydrous silicates on the surfaces. The meteorite collection contains no identifiable analogs to Trojan asteroids. Among small body populations, some Main Belt asteroids, comets, irregular satellites, and Centaurs provide reasonable spectral matches, supporting some genetic relationships among some members of these groups. The cause of the observed spectral properties remains uncertain, but recent suggestions include a combination of volatile ice sublimation and space weathering or a combination of impact gardening and space weathering. The Lucy mission will provide detailed compositional analysis of (3548) Eurybates, (15094) Polymele, (11351) Leucus, (21900) Orus, and (617) Patroclus-Menoetius, a suite of targets that sample the diversity among the Trojan population along several dimensions. With these flybys, the Lucy mission is poised to resolve many of the outstanding questions regarding Trojan surface compositions, thereby revealing how the Trojans formed and evolved and providing a clearer view of Solar System history
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Optimising Thermal Mapping Instrument Filters to Unveil Enceladus' Subsurface Secrets

Copernicus Publications (2024)

Authors:

Duncan Lyster, Carly Howett, Neil Bowles, Rory Evans, Tristram Warren, Keith Nowicki
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Tailoring Infrared Filters for Global Mapping of Enceladus' Surface Temperatures

Curran Associates (2024) 935-941

Authors:

Duncan Lyster, Carly Howett, Neil Bowles, Keith Nowicki, Rory Evans, Tristram Warren
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Helene's surface properties from a photometric multi-wavelength analysis

Icarus 392 (2023)

Authors:

E Royer, A Hendrix, J Elliott, L Esposito, C Howett, L Spilker

Abstract:

On January 31, 2011, the remote-sensing instruments onboard the Cassini spacecraft (UVIS (Ultraviolet Imaging Spectrograph; ISS (Imaging Science Subsystem); VIMS (Visual and Infrared Mapping Spectrometer) and CIRS (Composite Infrared Spectrometer)) observed Helene, Dione's leading Lagrangian moon. We report here on the photometric characteristics of Helene between 0.11 μm and 5.2 μm. We find that Helene's spectrum is dominated by the signature of water-ice and we retrieve a grain size of 3.4 μm in the ultraviolet. At all wavelengths, Helene shows signs of being a relatively fresh surface less affected by space weathering effects than other observed surfaces in the Saturn system. We present the first phase curve of Helene at 0.61 μm and place our ultraviolet and near-IR results in a wider spectral context toward a better understanding of Helene's surface evolution. Previous studies suggested that either a recent impact on Helene or an asymmetric flux of E-ring particles could explain the satellite high surface brightness (Hedman et al., 2020). Results from this study favor the impactor hypothesis to explain Helene's photometric behavior.
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L’Ralph: A Visible/Infrared Spectral Imager for the Lucy Mission to the Trojans

Space Science Reviews Springer 219:8 (2023) 69

Authors:

DC Reuter, AA Simon, A Lunsford, H Kaplan, M Garrison, J Simpson, G Casto, Z Dolch, P Finneran, W Grundy, C Howett, P Kim, M Loose, T Null, F Parong, J Rodriguez-ruiz, P Roming, K Smith, P Thompson, B Tokarcik, T Veach, S Wall, J Ward, E Weigle, H Levison

Abstract:

Abstract The Lucy Mission to the Trojan asteroids in Jupiter’s orbit carries an instrument named L’Ralph, a visible/near infrared multi-spectral imager and a short wavelength infrared hyperspectral imager. It is one of the core instruments on Lucy, NASA’s first mission to the Trojans. L’Ralph’s primary purpose is to map the surface geology and composition of these objects, but it will also be used to search for possible tenuous exospheres. It is compact, low mass (32.3 kg), power efficient (24.5 W), and robust with high sensitivity and excellent imaging. These characteristics, and its high degree of redundancy, make L’Ralph ideally suited to this long-duration multi-flyby reconnaissance mission.
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