Sep 7, 1999

Plasma, Plasma, Everywhere

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A new model of the plasmasphere
surrounding our world

Earth from Apollo 17
Sept. 7, 1999: As photographed from space, the Earth looks like it is floating in a black void. But, unseen by our eyes and most cameras, the Earth is actually surrounded by a complex system of interacting electric and magnetic fields, electric currents and charged particles called the magnetosphere.

Right: If a camera didn't compensate for the bright sunlight in space, stars would be seen in the background and the Earth would appear as a bright white orb. Because distant stars aren't as bright as the Earth, a low photo exposure results in a black background.

The magnetosphere provides a barrier between our planet and particles continually given off by the Sun's corona called the "solar wind." These particles constitute a plasma - a mixture of electrons (negatively charged) and ions (atoms that have lost electrons, resulting in a positive electric charge).

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Plasma is not a gas, liquid, or solid - it is the fourth state of matter. Plasma often behaves like a gas, except that it conducts electricity and is affected by magnetic fields. On an astronomical scale, plasma is common. The Sun is composed of plasma, fire is plasma, fluorescent and neon lights contain plasma.

"99.9 percent of the Universe is made up of plasma," says Dr. Dennis Gallagher, a plasma physicist at NASA's Marshall Space Flight Center. "Very little material in space is made of rock like the Earth."

Artist's concept of the shape of the magnetosphere
The plasma of the magnetosphere has many different levels of temperature and concentration. The coldest magnetospheric plasma is most often found in the plasmasphere, a donut-shaped region surrounding the Earth's middle. But plasma from the plasmasphere can be detected throughout the magnetosphere because it gets blown around by electric and magnetic forces.

Left: Artist's concept of the magnetosphere. The rounded, bullet-like shape represents the bow shock as the magnetosphere confronts solar winds. The area represented in gray, between the magnetosphere and the bow shock, is called the magnetopause. The Earth's magnetosphere extends about 10 Earth radii toward the Sun and perhaps similar distances outward on the flanks The magnetotail is thought to extend as far as 1,000 Earth radii away from the Sun.

Gallagher has developed a general model to describe the density of the plasma surrounding the Earth. His paper, "Global Core Plasma Model," will be published in the Journal of Geophysical Research. "Core plasma" refers to the low-energy plasma (zero to 100 electron volts) that makes up the plasmasphere.

The plasmasphere extends out to as little as 2 to 3 Earth radii and, under quiet conditions on the

click for an animation showing the shape of the magnetosphere
evening side, perhaps more than 6 Earth radii. (Because conditions in space constantly vary and regions never have exact boundaries, plasma physicists measure the plasmasphere relative to the size of Earth: 4,000 miles [6,400 km] is about one Earth radius.) The extent of the plasmasphere depends on space weather activity. High levels of activity erode the plasmasphere; long periods of quiet allow the plasmasphere to expand.

Right: Click the image for a 3D simulation of the magnetosphere's shape. The Sun is off screen to the left. The animation begins showing the Earth, which recedes as the shape and size of the magnetosphere comes into view. The solar wind deforms the magnetosphere into its characteristic shape. Where the magnetosphere and the solar wind meet is the "bow shock," represented in the animation by a faint, translucent bullet shape. Credit: Digital Radiance

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Rockets, satellites and the space shuttle have flown in parts of the core plasma neighborhood. By taking various measurements of this region, scientists have gradually come to understand the basic nature of the entire plasmasphere.

"We've been flying in plasma for over 40 years and have slowly gained a statistical picture of what things are like, such as the density and proportion of oxygen, hydrogen, and helium," says Gallagher.

But our understanding of the plasmasphere is not complete. For one thing, all the various measurements have resulted in many independent models of specific plasma regions. By combining previous work, Gallagher's model attempts to describe, mathematically, a general, complete image of the plasmasphere.

EVU prime1.GIF

Left: Animation of the Earth's plasmasphere as it would appear in extreme ultraviolet light (30.4 nm wavelength). This simulates the view from the IMAGE satellite due to launch in February 2000. To watch a QuickTime movie of this animation, .

"This model begins to paint a picture, but it's something of a Frankenstein's monster," says Gallagher, referring to how his model is pieced together from several different, dissimilar models. "A significant issue is how you smooth the stitches."

Gallagher's model combines the International Reference Ionosphere (IRI) model for low altitudes with higher altitude models. The part of our atmosphere that contains plasma - the ionosphere - is generally 90 to 1,000 km (54-620 mi.) above the ground.

Web Links
Space Plasma Physics - research on plasma at NASA's Marshall Space Flight Center.
Earth's Solar Environment - International Space Physics Educational Consortium.
Exploration of the Earth's Magnetosphere - overview of NASA research on the Earth's environment in space.
The shorter wavelengths of sunlight, ranging from the ultraviolet to X-rays, ionize the Earth's upper atmosphere by tearing electrons off atoms. The ions and electrons do not readily recombine in the ionosphere because particle collisions are infrequent in the rarified atmosphere. Ionospheric densities range from a peak of about 1 million particles/cm3 down to many thousands of particles/cm3. The densities continue to fall as you move to higher altitudes.

From the equator to the middle latitudes of Earth, the ionosphere joins smoothly with the plasmasphere. Beyond the outer boundary of the plasmasphere, the densities of plasma in the magnetosphere can fall as low as 0.01 particles/cm3.

"The plasma environment around the Earth is a natural extension of Earth's atmosphere, ionized by the Sun," says Gallagher. "Any planet that has an atmosphere is going to have energy from the Sun imparted to the atoms. The consequences are that lighter elements escape. But Earth's magnetic field traps much of this escaping gas. A planet like Mars that has, at best, a weak magnetic field, also has a very thin atmosphere. Some researchers have speculated that the Earth's magnetic field may pla

y a role in slowing the loss of our atmosphere into space."

Right: Artist's concept of the interaction between the magnetosphere and the Sun. The Earth's magnetic field provides a barrier to the solar wind.

Our atmosphere provides pressure, proper temperature, and oxygen - fundamental requirements for life on Earth. Without the atmosphere, one side of our planet would freeze while the other would broil under intense solar radiation.

Gallagher's model may contribute to our understanding of how the Earth's plasma affects our quality of life. Radio waves and power lines are affected by the presence of plasma, as are satellites and the Space Shuttle. Plasma can cause an electric charge to accumulate on one part of a spacecraft but not another, sometimes resulting in an electric arc, or discharge. These electric arcs can disrupt or destroy sensitive electronic components.

Gallagher will be able to refine his model with data from the IMAGE satellite, due to launch in February 2000. IMAGE will give us a better picture of the Earth's magnetosphere, and because plasma is bound to magnetic fields, IMAGE should also improve our understanding of how the plasmasphere and the magnetosphere interact.

More web links

Space Weather Camera Set for Launch in 2000 - Feb. 16, 1999

Imager for Magnetopause-to-Auroral Global Exploration (IMAGE) - satellite facts and objectives.

Space Physics Textbook - University of Oulu Space Research Group.

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For more information, please contact:
Dr. John M. Horack , Director of Science Communications
Author: Leslie Mullen
Curator: Linda Porter
NASA Official: M. Frank Rose