Coronal cloud

Solar Event
Coronal Cloud

An image of a coronal mass ejection, with the coronal cloud visible around it.
Overview
Name: Coronal Cloud
Type: Flare
Area: Chromosphere
Statistics
Average Size: 66,000-240,000 Km
Temperature: Same as Solar Flare
Occurrence Ratio: About 4 Times Per Day
See also, CME

A coronal cloud is the cloud of hot plasma gas surrounding a coronal mass ejection. It is usually made up of protons and electrons. When a coronal mass ejection occurs, it is the coronal cloud that usually reaches Earth and causes damage to electrical equipment and space satellites, not the ejection or flare itself. The damage is mostly the result of the high amount of electricity moving through the atmosphere.[1]

A coronal cloud is released when a solar flare becomes a coronal mass ejection; the coronal cloud often contains more radioactive particles than the mass ejection itself. A coronal mass ejection occurs when a solar flare becomes so hot that it snaps and breaks in two, becoming a "rope" of heat and magnetism that stretches between two sunspots. The resulting coronal mass ejection can be compared to a horseshoe magnet, the sunspots being the poles and the oscillating magnetic connector the handle. Coronal mass ejections typically do not last very long, because they cool down as the coronal cloud of gas is released and begins to hurtle away from the sun.[2]

Formation and solar detachment

An image of a coronal cloud, half expanded into space
An example of a coronal cloud at half expansion. The inner portion is still plasma with the magnetic rope visible, but the outer area is gaseous and already expanded quite far into space.

When a coronal cloud occurs, it can take several days for the plasma to grow cool enough to detach from the sun. This usually happens before the coronal mass ejection is able to cool enough for the magnetism to dissipate, at which point the solar flare cycle begins again. While the gas cloud is still cool enough to be in a semi-liquid plasma state, it clings tightly to the mass ejection, insulating it from the cold temperature of extra-solar space.[3]

As the outer edges of the cloud begin to cool, the mass ejection's magnetic rope begins to cool, thereby decentralizing what remains of the flare by weakening its magnetic pull. After the cloud begins to cool, it gradually cools further and further into its core. The mass ejection expands into space as its insulating cloud weakens, weakening the magnet even more. By this point, the sun spots are all but gone.[4]

When the coronal cloud changes completely from gas to liquid, the cycle of detachment begins. The inner, liquid plasma area of the cloud is relatively small and being heated by the mass ejection, not the other way around. The mass ejection loses its magnetism almost immediately, and cools to gas form or falls back into the sun within hours. However, the coronal cloud is still attached to it.[4]

The coronal cloud (no longer coronal) and what is left of the mass ejection detach from the sun. The cloud of gas, radioactive particles, and electrons, however, is still in the sun's gravitational pull. One of two things can happen:

If the cloud begins hurtling into space, it usually becomes trapped in the planets' orbital gravity. By the time it gets to Earth, enough of the cloud has been absorbed by Mercury and Venus that the Earth's magnetosphere can deflect what's left into the outer solar system. Occasionally, though, an abnormally large and fast cloud can pass a portion of its mass into the upper atmosphere.[5]I invented today the Struck Cloud to imitate Jan Oort and his Oort Cloud. The Struck Cloud is the area around the Sun that the sun's plasma forms a cloud like structure. To have a Struck Cloud, there does not need to be a coronal mass ejection. James T. Struck BA, BS, AA, MLIS

Effects

A magnetic cloud (as it is now termed) can travel toward Earth at speeds that can exceed 7,000,000 miles (11,000,000 km) per hour. On average, it usually takes them about 13½ hours to reach Earth. The cloud hurtling through space is called a solar wind. As many as five can be ejected from the sun during solar maximum. When they reach the Earth, the large amounts of radioactive and electric energy can temporarily disrupt or even destroy electrical grids, antennae, communications devices, electric appliances, and near anything electric.[2] Minor damage may also be done to living organisms due to the low level radiation that gets through the magnetosphere.[2]

Specific reasons as to why these clouds are dangerous to electronic and communication equipment include the overloading of large power transformers, which can cause lengthy power outages over wide geographical areas. Long, metallic structures like oil and gas pipes, water pipes, and communications antennae can also carry excessive electric current from the air, causing them to corrode faster than normal. This can possibly lead to early, unexpected ruptures. These signals also create anomalies in the ionosphere, disrupting wireless technologies such as GPS, cellular phones, television, and radio.[2]

Notable occurrences

A diagram of the November 17, 1882, "Transit of Venus Storm"
An image of the March 13, 1989, solar flare, which created a coronal cloud that took out power for 6 million people in Quebec and Ontario. Taken by the SOHO Space Telescope.
An Aurora Borealis as seen in South Dakota due to the June 16, 2012, coronal cloud. Auroras wereseen as far south as Ocean City, Maryland.

See also

References

  1. Manfred Kaiser (2007). "Coronal Mass Ejection". Global BioWeather Inc. Retrieved 2013-02-19.
  2. 1 2 3 4 5 N/A. "Space Weather: Sunspots, Solar Flares & Coronal Mass Ejections". TechMediaNetwork. Retrieved 2013-02-19.
  3. Tony Philips (2008-05-27). "Cartwheel Coronal Mass Ejection". NASA. Retrieved 2013-02-09.
  4. 1 2 Lin Yong; S.F. Martin; O. Engvold (June 2006). ""Coronal Cloud" Prominences And Their Association With Coronal Mass Ejections". Institute of Theoretical Astrophysics, Norway. Retrieved 2013-02-09.
  5. Australian Space Academy (2000). "Coronal Mass Ejections". Australian Space Academy. Retrieved 2013-02-09.
  6. Alexander McAdie (October 1897). "What is a Aurora?". Today in Science. Retrieved 2013-02-10.
  7. C. B. Henry (1882-11-17). "November 17, 1882 - The Transit of Venus Storm". The Kansas City Evening Star. Retrieved 2013-02-10.
  8. J. Douglas Kenyon (2012-03-01). Atlantis Rising Magazine - 92 March/April 2012. Atlantis Rising LLC. pp. 57–. ISBN 978-1-4675-0094-4.
  9. S. M. Silverman; E. W. Cliver (2001-01-01). "Low-latitude auroras: the magnetic storm of 14–15 May 1921". University of Nebraska Lincoln. Retrieved 2013-02-10.
  10. Adam Hadhazy (2009-03-13). "A Scary 13th: 20 Years Ago, Earth Was Blasted with a Massive Plume of Solar Plasma [Slide Show]". The Scientific American. Retrieved 2013-02-09.
  11. NASA (2003-10-23). "Solar Superstorm". NASA. Retrieved 2013-02-09.
  12. Sten Odenwald (2009-03-13). "The Day the Sun Brought Darkness". NASA. Retrieved 2013-02-09.
  13. Ruth Netting (2000-06-14). "A Solar Radiation Storm". NASA. Retrieved 2013-02-09.
  14. Lee Rannals (2012-06-15). "Incoming Coronal Mass Ejection Coming On June 16". redOrbit.com. Retrieved 2013-02-09.


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