The five largest moons of Uranus – sometimes called the “classical moons” -- appear in a jagged, roughly diagonal line from top right to bottom left. These are labeled Titania, Oberon, Umbriel, Miranda and Ariel. Also visible is Ariel’s shadow, which is superimposed on Uranus. Faint, ghostly, Saturn-like rings encircle the blue ice giant. Credits/Science: NASA, ESA, STScI, Christian Soto (STScI). Image Processing: Joseph DePasquale (STScI)
This image of Uranus and its five classical moons -- Titania, Oberon, Umbriel, Miranda and Ariel -- was captured by the Hubble Space Telescope’s. div style="text-align: justify;">Advanced Camera for Surveys (ACS). The image shows a scale bar, compass arrows, and color key for reference. The five largest moons of Uranus – sometimes called the “classical moons” -- appear in a jagged, roughly diagonal line from top right to bottom left. These are labeled Titania, Oberon, Umbriel, Miranda and Ariel. Also visible is Ariel’s shadow, which is superimposed on Uranus. Faint, ghostly, Saturn-like rings encircle the blue ice giant. Credits/Science: NASA, ESA, STScI, Christian Soto (STScI). Image Processing: Joseph DePasquale (STScI). The scale bar is labeled in miles along the top and kilometers along the bottom. The north and east compass arrows show the orientation of the image on the sky. Note that the relationship between north and east on the sky (as seen from below) is flipped relative to direction arrows on a map of the ground (as seen from above). This image shows visible wavelengths of light that have been translated into visible-light colors. The color key shows which ACS filters were used when collecting the light. The color of each filter name is the visible-light color used to represent the light that passes through that filter. Credits/Science: NASA, ESA, STScI, Christian Soto (STScI). Image Processing: Joseph DePasquale (STScI)
Scientists using NASA’s Hubble Space Telescope went looking for evidence of one phenomenon and found quite another.
The research team studied the four largest moons of the ice giant
Uranus, the seventh planet from our Sun, searching for signs of ,.
interactions between Uranus'
magnetosphere
and the surfaces of the moons. (A magnetosphere is a region surrounding
a celestial body where particles with an electrical charge are affected
by the astronomical object’s magnetic field.)
In particular, the team predicted that, based on interactions with
Uranus' magnetosphere, the “leading” sides of these tidally locked
moons, which always face in the same direction in which they are
orbiting the planet, would be brighter than the “trailing” sides, always
facing away. This would be due to radiation darkening of their trailing
sides by charged particles such as electrons trapped in Uranus’
magnetosphere.
Instead, they found no evidence for darkening on the moons’ trailing
sides, and clear evidence for darkening of the leading sides of the
outer moons. This surprised the team and indicates that Uranus’
magnetosphere might not interact much with its large moons,
contradicting existing data collected over near-infrared wavelengths.
Hubble’s sharp ultraviolet vision and
spectroscopic capabilities were critical for allowing the team to investigate the
surface conditions on these moons and uncover the surprising finding.
The Complicated Magnetic Environment of ‘Weird’ Uranus
The four moons in this study — Ariel, Umbriel, Titania, and Oberon —
are tidally locked to Uranus, so that they always show the same side to
the planet. The side of the moon facing the direction of travel is
called the leading hemisphere, while the side that faces backward is
called the trailing hemisphere. The thinking was that charged particles
trapped along the magnetic field lines primarily hit each moon’s
trailing side, which would darken that hemisphere.
“Uranus is weird, so it's always been uncertain how much the magnetic
field actually interacts with its satellites,” explained principal
investigator Richard Cartwright of the Johns Hopkins University’s
Applied Physics Laboratory. “For starters, it is tilted by 98 degrees
relative to the
ecliptic.”
This means Uranus is dramatically tipped relative to the orbital
plane of the planets. It rolls very slowly around the Sun on its side as
it completes its 84-Earth-year orbit.
“At the time of the Voyager 2 flyby, the magnetosphere of Uranus was
tilted by about 59 degrees from the orbital plane of the satellites. So,
there's an additional tilt to the magnetic field,” explained
Cartwright.
Because Uranus and its magnetic field lines rotate faster than its
moons orbit the planet, the magnetic field lines constantly sweep past
the moons. If the magnetosphere of Uranus interacts with its moons,
charged particles should preferentially hit the surface of the trailing
sides.
These charged particles, as well as our galaxy’s cosmic rays, should
darken the trailing hemispheres of Ariel, Umbriel, Titania, and Oberon
and possibly generate the carbon dioxide detected on these moons. The
team expected that, especially for the inner moons Ariel and Umbriel,
the trailing hemispheres would be darker than the leading sides in
ultraviolet and visible wavelengths.
But that’s not what they found. Instead, the leading and trailing
hemispheres of Ariel and Umbriel are actually very similar in
brightness. However, the researchers did see a difference between the
hemispheres of the two outer moons, Titania and Oberon — not the moons they expected.
Like Bugs on a WindshieldEven stranger, the difference in brightness was the opposite of what
they expected. The two outer moons have darker and redder leading
hemispheres compared with their trailing hemispheres. The team thinks
that dust from some of Uranus’ irregular satellites is coating the
leading sides of Titania and Oberon.
Irregular satellites are natural bodies that have large, eccentric,
and inclined orbits relative to their parent planet’s equatorial plane.
Micrometeorites are constantly hitting the surfaces of Uranus’ irregular
satellites, ejecting small bits of material into orbit around the
planet.
Over millions of years, this dusty material moves inward toward
Uranus and eventually crosses the orbits of Titania and Oberon. These
outer moons sweep through the dust and pick it up primarily on their
leading hemispheres, which face forward. It's much like bugs hitting the
windshield of your car as you drive down a highway.
This material causes Titania and Oberon to have darker and redder
leading hemispheres. These outer moons effectively shield the inner
moons Ariel and Umbriel from the dust, which is why the inner moons’
hemispheres do not show a difference in brightness.
“We see the same thing happening in the Saturn system and probably
the Jupiter system as well,” said co-investigator Bryan Holler of the
Space Telescope Science Institute. “This is some of the first evidence
we’re seeing of a similar material exchange among the Uranian
satellites.”
“So that supports a different explanation,” said Cartwright. “That's
dust collection. I didn't even expect to get into that hypothesis, but
you know, data always surprise you.”
Based on these findings, Cartwright and his team suspect that Uranus'
magnetosphere may be fairly quiescent, or it may be more complicated
than previously thought. Perhaps interactions between Uranus' moons and
magnetosphere are happening, but for some reason, they’re not causing
asymmetry in the leading and trailing hemispheres as researchers
suspected. The answer will require further investigation into enigmatic
Uranus, its magnetosphere, and its moons.
Hubble’s Unique Ultraviolet VisionTo observe the brightnesses of the four largest Uranian moons, the
researchers required Hubble’s unique ultraviolet capabilities. Observing
targets in ultraviolet light is not possible from the ground because of
the filtering effects of Earth’s protective atmosphere. No other
present-day space telescopes have comparable ultraviolet vision and
sharpness.
“Hubble, with its ultraviolet capabilities, is the only facility that
could test our hypothesis,” said the Space Telescope Science
Institute’s Christian Soto, who conducted much of the data extraction
and analysis. Soto presented results from this study on June 10 at the
246th Meeting of American Astronomical Society in Anchorage, Alaska.
Complementary data from NASA’s James Webb Space Telescope will help
to provide a more comprehensive understanding of the Uranian satellite
system and its interactions with the planet’s magnetosphere.
The Hubble Space Telescope has been operating for over three decades
and continues to make ground-breaking discoveries that shape our
fundamental understanding of the universe. Hubble is a project of
international cooperation between NASA and ESA (European Space Agency).
NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the
telescope and mission operations. Lockheed Martin Space, based in
Denver, also supports mission operations at Goddard. The Space Telescope
Science Institute in Baltimore, which is operated by the Association of
Universities for Research in Astronomy, conducts Hubble science
operations for NASA.
The Space Telescope Science Institute is expanding the frontiers of
space astronomy by hosting the science operations center of the Hubble
Space Telescope, the science and mission operations centers for the
James Webb Space Telescope, and the science operations center for the
Nancy Grace Roman Space Telescope. STScI also houses the Barbara A.
Mikulski Archive for Space Telescopes (MAST) which is a NASA-funded
project to support and provide to the astronomical community a variety
of astronomical data archives, and is the data repository for the
Hubble, Webb, Roman, Kepler, K2, TESS missions and more. STScI is
operated by the Association of Universities for Research in Astronomy in
Washington, D.C.
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