78 research outputs found
The Science Case for a Return to Enceladus
The plume of Enceladus is unique in the solar system in providing direct access to fresh material from an
extraterrestrial subsurface ocean. The Cassini Mission, though not specifically designed for it, was able to take
advantage of the plume to conduct the best characterization to date of an extraterrestrial ocean. Evidence gathered
from multiple instruments points to a global, subsurface liquid water ocean rich in salts and organic compounds,
with water-rock interactions occurring presumably in hydrothermal systems at or below the moon’s sea floor.
Meeting the criteria of “extended regions of liquid water, conditions favorable for the assembly of complex organic
molecules, and energy source(s) to sustain metabolism,” the ocean of Enceladus can therefore be considered
habitable. It is also the only confirmed place beyond the Earth where we can easily sample fresh material from a
demonstrably habitable environment without the complications of digging or drilling. The next step is to
investigate whether Enceladus’ ocean is actually inhabited. Here, we summarize the evidence for Enceladus’ ocean
and its habitability, identify constraints and outstanding questions on the detectability of life within its ocean, and
recommend a return to Enceladus with a dedicated search-for-life mission (or missions)
The Saturn Ring Skimmer Mission Concept: The next step to explore Saturn's rings, atmosphere, interior, and inner magnetosphere
The innovative Saturn Ring Skimmer mission concept enables a wide range of
investigations that address fundamental questions about Saturn and its rings,
as well as giant planets and astrophysical disk systems in general. This
mission would provide new insights into the dynamical processes that operate in
astrophysical disk systems by observing individual particles in Saturn's rings
for the first time. The Ring Skimmer would also constrain the origin, history,
and fate of Saturn's rings by determining their compositional evolution and
material transport rates. In addition, the Ring Skimmer would reveal how the
rings, magnetosphere, and planet operate as an inter-connected system by making
direct measurements of the ring's atmosphere, Saturn's inner magnetosphere and
the material owing from the rings into the planet. At the same time, this
mission would clarify the dynamical processes operating in the planet's visible
atmosphere and deep interior by making extensive high-resolution observations
of cloud features and repeated measurements of the planet's extremely dynamic
gravitational field. Given the scientific potential of this basic mission
concept, we advocate that it be studied in depth as a potential option for the
New Frontiers program.Comment: White paper submitted to the Planetary Science and Astrobiology
Decadal Survey (submission #420
The Saturn Ring Skimmer Mission Concept: The next step to explore Saturn's rings, atmosphere, interior and inner magnetosphere
The innovative Saturn Ring Skimmer mission concept enables a wide range of investigations that address fundamental questions about Saturn and its rings, as well as giant planets and astrophysical disk systems in general. This mission would provide new insights into the dynamical processes that operate in astrophysical disk systems by observing individual particles in Saturn's rings for the first time. The Ring Skimmer would also constrain the origin, history, and fate of Saturn's rings by determining their compositional evolution and material transport rates. In addition, the Ring Skimmer would reveal how the rings, magnetosphere, and planet operate as an inter-connected system by making direct measurements of the ring's atmosphere, Saturn's inner magnetosphere and the material owing from the rings into the planet. At the same time, this mission would clarify the dynamical processes operating in the planet's visible atmosphere and deep interior by making extensive high-resolution observations of cloud features and repeated measurements of the planet's extremely dynamic gravitational field. Given the scientific potential of this basic mission concept, we advocate that it be studied in depth as a potential option for the New Frontiers program
The ALMA-CRISTAL survey: Widespread dust-obscured star formation in typical star-forming galaxies at z=4-6
We present the morphological parameters and global properties of
dust-obscured star formation in typical star-forming galaxies at z=4-6. Among
26 galaxies composed of 20 galaxies observed by the Cycle-8 ALMA Large Program,
CRISTAL, and six galaxies from archival data, we have individually detected
rest-frame 158m dust continuum emission from 19 galaxies, nine of which
are reported for the first time. The derived far-infrared luminosities are in
the range 10.9-12.4, an order of magnitude
lower than previously detected massive dusty star-forming galaxies (DSFGs). The
average relationship between the fraction of dust-obscured star formation
() and the stellar mass is consistent with previous results at
z=4-6 in a mass range of 9.5-11.0 and show
potential evolution from z=6-9. The individual exhibits a
significant diversity, and it shows a correlation with the spatial offset
between the dust and the UV continuum, suggesting the inhomogeneous dust
reddening may cause the source-to-source scatter in . The
effective radii of the dust emission are on average 1.5 kpc and are
times more extended than the rest-frame UV. The infrared surface
densities of these galaxies () are one order of magnitude
lower than those of DSFGs that host compact central starbursts. On the basis of
the comparable contribution of dust-obscured and dust-unobscured star formation
along with their similar spatial extent, we suggest that typical star-forming
galaxies at z=4-6 form stars throughout the entirety of their disks
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