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Plasma Clouds

Plasma clouds

Encircling the equatorial region of the Earth, and extending to latitudes nearly as far as the Arctic Circle, are regions of space where powerful flows of particles exist. Since the late 1950s at the dawn of the Space Age, they have been called the Van Allen belts. They were at one time believed to be particles from the solar wind, trapped by the Earth's magnetic field.

 

There are actually two belts which are shaped like two nested donuts centered on the Earth. The inner belt contains 10 million-volt, high-energy protons (the stripped nuclei of hydrogen atoms), and is located between 700 kilometers and 12,000 kilometers from the Earth's surface. The outer belt contains mostly electrons with energies higher than 1 million volts, located between 25,000 and 40,000 kilometers from the Earth's surface.

 

There are two other important systems of particles that invisibly orbit the Earth: the plasmasphere and the ring current. Both of these systems contain much lower energy particles than the Van Allen belts, although they occupy nearly the same regions of space extending to at least 45,000 kilometers from the Earth's surface.

Low-energy particles, with energies of a few tens of volts, surround the Earth in a vast donut-shaped cloud called the plasmasphere. The Earth's magnetic field in this region is so strong that the charged plasmasphere particles are pulled along with the Earth's 24-hour rotation.

 

During times of severe coronal mass ejections, atoms from the Earth's atmosphere are actually pumped into the plasmasphere in a so-called polar fountain. These fountains can be detected by orbiting satellites as they pass through the arctic and antarctic regions within a few thousand kilometers of the Earth.

 

The ring current extends from 8,000 kilometers to nearly 30,000 kilometers from the surface and occupies nearly the same zone as the much more energetic Van Allen belts. Ring current particles carry energies of thousands of volts. It is not a complete equatorial ring, like the planet Saturn's rings, but is only at its strongest on the night-side of the Earth. Its strength increases and decreases with the activity in the magnetotail region.

Source:NASA

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