The Earth's Plasmasphere



This image is a summary of the main features of the plasmasphere: the plasmapause, main body of the plasmasphere, dusk-bulge region and detached plasma regions outside the main body of the plasmasphere
Click on image for full size (75K JPEG)
The plasmasphere is a torus-shaped region within the Earth's magnetosphere. The Earth's plasmasphere is made of just that - plasma. It has a very sharp edge called the plasmapause at equatorial distances of 4-6 Earth radii. The plasmapause, where densities drop by a factor of 10-100 in a relatively short distance, was discovered in 1963.

The plasmasphere is essentially an extension of the ionosphere to high altitudes. Inside of the plasmapause, geomagnetic field lines rotate with the Earth. Plasma, flowing up from the ionosphere, is trapped on these corotating field lines and builds up to high densities. Outside the plasmapause, magnetic field lines are unable to corotate because they are influenced strongly by electric fields of solar wind origin. They convect to the magnetopause boundary on the day side of the Earth, sweeping the ionospheric plasma out of the magnetosphere and forming the sharp plasmasphere boundary. The plasmasphere bulges out to greater distances on the dusk side of the Earth.

The plasmasphere is composed mostly of hydrogen ions. The plasma density ranges from 104 cm-3 just above the topside ionosphere to 102 cm-3 within and 10 cm-3 just exterior to the plasmapause. The base of the plasmasphere is taken as the altitude (~ 1000 kilometers) at which protons replace oxygen as the dominant species in the ionospheric plasma. The ion temperature in the plasmasphere is generally between 0.5 eV and several eV (1 eV = 11,700 K).

What is a Magnetosphere?



The Earth's Plasmasphere



This image is a summary of the main features of the plasmasphere: the plasmapause, main body of the plasmasphere, dusk-bulge region and detached plasma regions outside the main body of the plasmasphere
Click on image for full size (75K JPEG)
The plasmasphere is a donut-shaped region inside the Earth's magnetosphere. It is basically an extension of the ionosphere, or the topmost part of the Earth's atmosphere. The magnetic field lines of the Earth capture plasma that flows up from the ionosphere, so that there is a plasma build-up. Scientists call that plasma build-up the plasmasphere.

The plasmasphere is composed mostly of hydrogen ions. The base of the plasmasphere, which is the same as the top of the ionosphere, is about 1000 kilometers from the Earth's surface. The temperature in the plasmasphere is generally between 6000K and 35,100K or VERY hot compared to temperatures we are used to!

The plasmasphere has a very sharp edge called the plasmapause. The plasmapause was discovered in 1963.

What is a Magnetosphere?



The Earth's Plasmasphere



This image is a summary of the main features of the plasmasphere: the plasmapause, main body of the plasmasphere, dusk-bulge region and detached plasma regions outside the main body of the plasmasphere
Click on image for full size (75K JPEG)
You may have heard your teacher talk about the 4 states of matter. Do you remember what they are? Solids (like your desk), liquids (like the milk you pour in your cereal), gases (like the air you blow into a balloon) and...plasma!

The Earth is actually surrounded by plasma! If you look at the picture to the left, the blue ring is all plasma. It's like the Earth is surrounded by an inner tube made up of plasma...or maybe you'd like to call it a plasma donut. Scientists have a big word for this inner tube or plamsa donut - the plasmasphere.

What is a Magnetosphere?




Last modified December 2, 1995 by the Windows Team

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