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Earth Structure Illustration Credit: Courtesy of Royal Observatory of Belgium |
An article in Nature Geoscience on the rotation of the Earth’s core (more precisely its solid inner core) was recently published. However, the media have been misled by the press release of the science journal into thinking that the inner core stopped rotating or was even rotating in the opposite direction to that of the Earth surface, which is not the case at all. Scientists of the Royal Observatory of Belgium specialized in the rotation of the Earth and planets clarify the study and provide some information on the structure and rotation of the Earth.
Internal structure and rotation of the Earth
The interior of the Earth is divided into concentric layers. A few tens of kilometers below the surface begins the solid mantle, which extends to a depth of about 2900 km. Below that is the Earth’s core, which consists mainly of iron. The core is subdivided into an upper liquid layer down to a depth of about 5150 km and a central solid inner core with a radius of about 1220 km. The article in Nature Geoscience article is about the solid inner core.
The Earth revolves around its axis of rotation in 24 hours. Movements in the Earth’s atmosphere, hydrosphere and liquid core can cause small variations in the rotational period, so-called “length-of-day variations”, which can be on the order of milliseconds. The different layers that make up the Earth are linked by gravity and the frictional force and the electromagnetic force between the core and the solid parts. Therefore, the rotational period of the solid inner core can show small variations compared to the rotation of the mantle.