Aurora: Sheets and waves of vibrant light caused by charged solar particles
igniting gases in Earth's atmosphere. They are typically visible
at northern latitudes, and sometimes (during heavy solar activity)
into the mid-latitudes of the United States and elsewhere. In-depth
look at the aurora
Geomagnetic
storm: When unusually strong surges of solar wind (charged particles
from the Sun) hit the Earth. This effect causes variations in
the magnetic field which surrounds the Earth. The result are visible
aurora (Northern and Southern lights).
Heliosphere: Charged particles streaming away from the Sun envelop Earth and
the other planets in a magnetic bubble. "The heliosphere
is the bubble this solar wind blows out into the local interstellar
medium. It defines the volume of space over which our Sun's influence
predominates," says Richard Marsden, the ESA's Ulysses project
scientist.
The closest
boundary of the heliosphere is thought to extend about 100 AU
out from the Sun, which is 100 times the distance of the Earth
from the Sun. The heliosphere protects us from the worst space
weather -- cosmic rays. These very energetic particles are generated
far away in the universe, and if not for our protective bubble,
they would bombard Earth continuously and damage living cells.
"Without the heliosphere, life would certainly have evolved
differentlyand maybe not at all," Marsden says. The
heliosphere is shaped and recharged by the solar wind.
Hot plasma trapped in magnetic loops.
Magnetic
Field: A field of force that is generated by electric currents. The Sun's
average large-scale magnetic field, like that of the Earth, exhibits
a north and a south pole linked by lines of magnetic force.
Solar
flare: The Sun frequently spews plumes of energy that are more energetic
than the constant solar wind. These solar flares contain gamma
rays and X-rays, plus energized particles (protons and electrons).
Energy can be equal to a billion megatons of TNT is released in
a matter of minutes. Flare activity picks up as sunspots increase.
The magnetic
explosion during a solar flare accelerates electrons and atomic
nuclei to significant fractions of the speed of light. Unlike
much slower atomic particles in the solar wind, which travel straight
out from the Sun, the energetic particles from a flare follow
curved lines of the Sun's interplanetary magnetic field. The particles
slant in toward Earth from the west at about 45 degrees to the
direction of the Sun.
Solar
flare classification: Solar flares are classified based on their output of X-ray energy
at the peak of their burst.
* C-class flares are common
* M-class flares are larger but moderately powerful
* X-class flares are the most powerful
More
detail on flare classification
Solar
wind: Charged particles, mostly protons and electrons, streaming out
from the Sun. Earth's own protective magnetic field repels most
of the solar wind. This stream of outflowing particles comes in
two varieties, "fast" (about 750 km/s) and "slow"
(350 to 400 km/s).
Solar wind
speed varies with solar latitude and solar activity. During periods
of low activity, the fast wind emanates from the poles and the
slow wind from near the equator. The fast wind comes from relatively
cool gaps in the corona, called coronal holes, and the slow wind
from hotter coronal "streamers". The solar wind feeds
the Sun's heliosphere.
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