New research provides the first-ever model of our Moon's rotational dynamics, taking into consideration its solid inner core. Their model helps to explain why, as seen from Earth, the Moon appears to wobble on its axis.
The Moon goes around the Earth, but its orbit is inclined by about five degrees with respect to the normal to the ecliptic plane, the plane about which Earth rotates around the Sun. But just like the Earth's rotation axis is inclined by 23.5 degrees in space, the Moon's rotation axis is also inclined, by about 1.5 degrees
Over one orbit, it points at the same direction in space, which is in the same plane as the normal to the orbit of the moon. This defines a Cassini state. This type of lunar orbit was first observed by Giovanni Cassini more than four centuries ago. Since that time, the complex mathematical and physical elements of the Cassini state have been examined by scientists around the world. But what makes this model unique is accounting for a solid inner core at the center of the Moon.
The researchers determined that the inner core is tilted as much as 17 degrees away from the mantle in one direction or 33 degrees away in the other. And, if scientists can identify the angle of the inner core, they will be able to develop a more accurate picture of the interior of the Moon.
This is the first model of the rotational dynamics of the Moon that fully takes into account the presence of a solid inner core. Understanding the composition of the Moon's interior may provide insight to the events leading up to the formation of the Moon and the early history of the Earth.