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Van Allen
The Van Allen radiation belts
the belts result from charged particles interacting with the magnetic field of the earth and incurring an inward force pulling it into a tighter and tighter spiral as it penetrates deeper into the earth's atmosphere.finally its forward motion is reversed and the particle spirals along the magnetic force line to the other end where a similar reflection occurs. the magnetic field axis is rotated eastward from the geographical axis which provides an unsymetrical magnetic particle distribution in the earth coordinate. solar flares cause large asymmeries in the particle distribution and potentially harmful damage to exposed skin,electronics and particle detectors.
In the upper atmosphere usually in latitudes above 50 degrees.
Jet Stream
The Van Allen belts are caused by Earth's magnetic field. Charged particles are deflected in the presence of a magnetic field.
Van Allen belts
Such areas are called Van Allen belts.
The charged particles flowing through space around the Earth follow the lines of magnetic force, resulting in a higher concentration of these particles in two toroidal bands curving outward from pole to pole. The radiation belts are called the Van Allen Belts after scientist James Van Allen (1914-2006).
the van Allen belts are located in the universal space.
magnetosphere
The Van Allen belts are composed of charged particles from the solar wind that became captured in the Earth's magnetic field. Deflection of charged particles
covection of the atom
The donut shaped radiation belts around the Earth are called the Van Allen Belts. There are similar belts around every planet with a magnetic field.
The Van Allen radiation belts are layers of plasma particles that are around the earth in the magnetosphere. These radiation belts were confirmed to exist in 1958 by James Van Allen. There is an outer and inner belt. The belts can cause problems for both satellites and any rockets or other vehicles that travel through the belts.
Those are the Van Allen belts.
The Van Allen belts.