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An Oddly Tilted Planet




The rotation period of Uranus’s atmosphere is about 16 hours.
Like Jupiter and Saturn, Uranus rotates differentially, so this period
depends on the latitude. This can be measured by tracking
the motions of clouds. To determine the rotation period for the
underlying body of the planet, scientists looked to Uranus’s magnetic
field, which is presumably anchored in the planet’s interior,
or at least in the deeper and denser layers of its atmosphere. Data
from Voyager 2 indicate that Uranus’s internal period of rotation
is 17.24 hours.
Voyager 2 also confirmed that Uranus’s rotation axis is tilted
in a unique and bizarre way. Herschel found the first evidence of
this in 1787, when he discovered two moons orbiting Uranus in
a plane that is almost perpendicular to the plane of the planet’s
orbit around the Sun. Because the large moons of Jupiter and Saturn
were known to orbit in the same plane as their planet’s equator
and in the same direction as their planet’s rotation, it was
thought that the same must be true for the moons of Uranus.




Thus, Uranus’s equator must be almost perpendicular to the plane
of its orbit, and its rotation axis must lie very nearly in that plane
(Figure 14-3).
Careful measurement shows that Uranus’s axis of rotation is
tilted by 98°, as compared to 231⁄2° for Earth (compare Figure
14-3 with Figure 2-12). A tilt angle greater than 90° means that Uranus exhibits retrograde (backward) rotation like that of Venus,
shown in Figure 11-7b. Astronomers suspect that Uranus might
have acquired its large tilt angle billions of years ago, when another
massive body collided with Uranus while the planet was still
forming. The radical tilt of its axis means that as Uranus moves along
its 84-year orbit, its north and south poles alternately point toward
or away from the Sun. This produces highly exaggerated
seasonal changes. For example, when Voyager 2 flew by in 1986,
Uranus’s south pole was pointed toward the Sun. Most of the
planet’s southern hemisphere was bathed in continuous sunlight,
while most of the northern hemisphere was subjected to a continuous,
frigid winter night. But over the following quarter of a
Uranian year later (21 of our years), sunlight has gradually been
returning to the northern hemisphere, triggering immense storms
there. Figure 14-2 shows some of these storms, which are much
more visible at infrared wavelengths than with visible light.

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