A Global Dataset of Potential Chloride Deposits on Mars as Identified by TGO CaSSIS
Scientific Data,
Год журнала:
2024,
Номер
11(1)
Опубликована: Авг. 3, 2024
Abstract
Chloride
deposits
are
markers
for
early
Mars’
aqueous
past,
with
important
implications
our
understanding
of
the
martian
climate
and
habitability.
The
Colour
Stereo
Surface
Imaging
System
(CaSSIS)
onboard
ESA’s
Trace
Gas
Orbiter
provides
high-resolution
color-infrared
images,
enabling
a
planet-wide
search
(small)
potentially
chloride-bearing
deposits.
Here,
we
use
neural
network
to
map
in
CaSSIS
images
over
significant
fraction
planet.
We
identify
965
chloride
deposit
candidates
diameters
ranging
from
<300
>3000
m,
including
previously
unknown
deposits,
136
(~14%)
which
located
highlands
north
equator,
up
~36°N.
Northern
tend
be
smaller
than
south
predominantly
small-scale
topographic
depressions
low-albedo
Noachian
Hesperian
highland
terranes.
Our
new
dataset
augments
existing
maps,
informs
current
future
imaging
campaigns,
enables
modelling
work
towards
better
distribution
near-surface
water
distant
past.
Язык: Английский
Albedo analysis of dust devil-induced slope streaks and tracks on Mars
Icarus,
Год журнала:
2024,
Номер
423, С. 116270 - 116270
Опубликована: Авг. 22, 2024
Язык: Английский
Novel quantitative methods to enable multispectral identification of high-purity water ice exposures on Mars using High Resolution Imaging Science Experiment (HiRISE) images
Icarus,
Год журнала:
2023,
Номер
419, С. 115849 - 115849
Опубликована: Ноя. 4, 2023
Язык: Английский
Geometric processing of TGO CaSSIS observations
Planetary and Space Science,
Год журнала:
2022,
Номер
223, С. 105581 - 105581
Опубликована: Окт. 19, 2022
Язык: Английский
A global map of gullied hillslopes on Mars
Icarus,
Год журнала:
2024,
Номер
418, С. 116147 - 116147
Опубликована: Май 26, 2024
The
distribution
of
gullies
on
Mars
has
been
used
to
support
different
modes
formation
involving
CO2,
H2O
or
entirely
dry
processes.
We
mapped
the
extent
gullied
hillslope
using
a
global
mosaic
ConTeXt
camera
(CTX)
at
6
m/pixel
and
High
Resolution
Imaging
Science
Experiment
(HiRISE)
browse
products
~3
m/pixel.
Our
new
globalcatalog
hillslopes
allows
for
quantitative,
area-based
analysis
both
regional
scale,
which
was
not
possible
with
point-based
more
localized
previous
datasets.
analyzed
aspect
gradient
information
derived
from
MOLA
topography
every
hillslope.
have
confirmed
trends
identified
in
works,
are
that
mean
is
lower
than
30°,
angle
repose
material
Mars,
preferred
latitude-dependent,
shift
between
pole-facing
equator-facing
happening
around
40°
hemispheres.
established
hierarchy
factors
can
explain
hillslopes:
Latitude
strictest
control
because
constrained
26°-83°S
28°-76°N.
availability
steep
slopes
strong
over
gully
distribution,
we
observed
reflects
orientation
large
reliefs,
implies
less
factor
explaining
distribution.
correlation
subsurface
water
ice
consistency
map,
found
preferentially
distributed
areas
some
ground
rather
no
all.
first
time
bias
toward
an
east-facing
trend
southern
hemisphere
poleward
~40°
latitude.
also
linked
our
dataset
crater
morphometry
dataset:
63%
area
craters,
find
covered
by
given
positively
correlated
depth
diameter
ratio
this
crater.
observations
point
complex
interplay
local
slope,
insolation,
thermal
properties
substrate
spatial
current
population
gullies.
Finally,
assessed
very
high
resolution
(sub-meter)
imagery
coverage
be
36%
repeated
reaches
21%
gullies,
hence
would
need
expanding
better
understand
active
Язык: Английский
Seasonal and Short Timescale Changes on the Martian Surface: Multi-Spacecraft Perspectives
Space Science Reviews,
Год журнала:
2024,
Номер
221(1)
Опубликована: Дек. 19, 2024
Abstract
The
continued
operation
of
missions
such
as
Mars
Express,
Reconnaissance
Orbiter,
and
the
ExoMars
Trace
Gas
Orbiter
has
greatly
enhanced
our
knowledge
seasonal
processes
on
Mars.
most
apparent
evidence
importance
seasons
large
scale
is
annual
variation
in
sizes
Martian
polar
caps.
However,
high
resolution
imaging
also
shown
that
forcing
can
lead
to
small-scale
phenomena
are
continuously
changing
topography
surface
photometry.
These
often
have
no
terrestrial
analogue
involve
complex
interactions
between
ices,
atmosphere,
substrate
(surface
sub-surface).
Although
we
now
better
understanding
many
these
(occasionally
a
result
laboratory
simulation),
direct
proof
some
hypotheses
remains
elusive.
We
provide
brief
review
list
series
open
questions.
Язык: Английский