“Progress in Understanding thePluto System: Ten Years after Flyby” was a focused, informative conference in
which scientists spent four-and-a-half days discussing Pluto in detail,
comparing it with other, similar solar system bodies, and celebrating the
milestone 10th anniversary of the 2015 New Horizons flyby.
Alan Stern, New Horizons principal
investigator, opened the conference by describing its goal as “bringing
together everything we’ve learned about the Pluto system since the flyby.”
Because so much ground was covered
during the weeklong, conference, it would be impossible to discuss everything
in one entry, which is why I plan to write several for this site.
In the first session, “Pluto after Ten
Years: A Holistic View,” discussion centered on Pluto’s climate, geological
history, atmosphere, and chemistry. A second session focused on the geology and
composition of Pluto’s largest moon and binary companion, Charon.
Throughout the conference, Pluto
and its system of moons were compared and contrasted with Ceres, Haumea, Eris, Arrokoth,
other Trans-Neptunian Objects and small planets, Neptune’s moon Triton, Saturn’s
moons Titan and Enceladus, and Jupiter’s moon Europa.
While little is known about Haumea
and Eris, every other one of these worlds is either an ocean world or a world
suspected of having a subsurface ocean. This class of objects was relatively
unknown just decades ago, but today, these worlds are front and center in the
search for microbial life in the solar system.
In the lead up to the flyby, some
scientists expected Pluto to be revealed as a geologically dead world, like our
moon. Instead, many were surprised to find it, in the words of presenter Oliver
White, “a geological wonderland at the edge of the solar system.”
Much focus was placed on Sputnik
Planitia, the floating glacier that comprises the left side of Pluto’s “heart”
feature, and the repository of the planet’s nitrogen ice. We know Sputnik
Planitia is geologically young, has nitrogen ice flowing on its surface, and
has no craters.
The flow of ice on Sputnik Planitia
is similar to processes on Earth, but with nitrogen ice instead of water.
Pluto’s annual cycle is driven by
the planet’s high obliquity or tilt toward the plane in which most but not all
of the solar system’s planets orbit. Its north-facing slopes all have small
deposits of methane ice. Over thousands of Pluto years, its equatorial regions
have received less sunlight than its polar regions.
Pluto’s diverse geology, including
bladed terrains, dunes, pitted regions, and even likely cryovolcanoes are the
result of both endogenic, or internal, processes, and exogenic, or external
ones.
The New Horizons team did not even
know that Sputnik Planitia was there when the flyby was planned. Since this
region controls almost everything that occurs on the planet, the opportunity to
image it in high resolution was extremely fortuitous.
Not being a satellite of a giant
planet, Pluto experiences no tidal heating. Its biggest source of energy is
radioactive decay of rock.
The ancient impact that formed
Charon melted ice, fractured terrain, and created Sputnik Planitia.
While the presence of a subsurface
ocean on Pluto remains hypothetical, it is supported by a lot of evidence.
Presenter James Tuttle Keane noted that a structure like Sputnik Planitia
cannot have been created without an ocean.
Computer models are frequently used
in studies to simulate conditions on remote objects like Pluto. Keane noted
that “New Horizons triggered a wave of new theoretical models reshaping our
understanding of Pluto and worlds beyond.”
Its axial tilt and eccentric orbit
give Pluto extreme summers and winters. Its lower latitudes get at least some
sunlight every day while its higher latitudes can go for long durations with no
sunlight at all. These differing climates produce a variety of landscapes on
Pluto’s surface.
But sunlight is not the only energy
source on Pluto, which obtains a higher fraction of its energy from internal
sources than the Earth does.
New Horizons found that Pluto’s
atmosphere is escaping into space at a much lower rate than expected.
Much discussion centered on early
migration of solar system planets. Neptune is believed to have formed closer to
the Sun only to subsequently migrate outward. Now located at 39 AU
(astronomical units, with one AU equal to 93 million miles or the average
Earth-Sun distance), Pluto may have formed at 25 AU and then been pushed
outward by Neptune.
Data obtained when various small
planets occulted (passed in front of) a star indicate that Pluto, Charon, Haumea,
Triton, and Quaoar all have similar densities.
“These objects are not iceballs,”
emphasized presenter Bill McKinnon, a point that supports their classification
as small planets. This is significant in light of the fact that the media often
erroneously lump dwarf planets and tiny Kuiper Belt Objects (KBOs) in one broad
category.
And KBOs, even those too small to
be round, are not just giant comets—they are far more active than comets are.
Pluto’s atmosphere is similar to
that of Saturn’s moon Titan, which itself is sometimes viewed as an analogue of
early Earth. Its surface ices are methane, nitrogen, and carbon monoxide.
Photochemical organic aerosols in Pluto’s atmosphere create its layered hazes,
which extend to an altitude of more than 217 miles.
Both Pluto and Triton, Neptune’s
large moon that is believed to have once orbited the Sun on its own only to be
captured by Neptune, look very different from comets. Rather than being frozen
relics, both have interior energy sources. Because Triton orbits Neptune, a
giant planet, it experiences far more tidal heating than Pluto.
Pluto and Triton have low levels of
carbon monoxide in their surface ices. Data collected by the James Webb Space
Telescope (JWST) show Eris and Makemake also lack surface carbon monoxide. As
neither orbit a giant planet, their surfaces may be more like that of Pluto
than that of Triton.
Since Triton is believed to have
originated in the Kuiper Belt, all of this is evidence that supports classing
these objects as a new subclass of planets, similar to one another but different
from comets.
The distribution of ices on Pluto’s
surface varies with its terrains. Nitrogen frost is found at the bottom of
craters. Bright and dark regions on Pluto have different ice compositions.
Data collected by New Horizons’
MVIC and LEISA instruments was used in 2023 to create spectral maps of Sputnik
Planitia, Cthulhu Macula, and Lowell Regio, regions on Pluto’s surface.
A global topography map of Pluto
created in 2018 used data from New Horizons and stellar occultations to depict
the distribution of volatiles, chemical elements and compounds that can be
easily vaporized.
Three regions on Pluto—Kiladze,
Viking Terra, and Virgil Fossae—could be cryovolcanoes. These resemble
structures on Mars known to be cryogenic caldera, or depressions formed by
cryovolcanism.
While Pluto’s topography is
current, Charon’s is ancient. Charon may have experienced tectonics, processes
that shape and create a planet’s crust, early in its history. While it may have
once had a subsurface ocean, that has long since frozen solid.