Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Aurora
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
=== Auroral particles === The immediate cause of the ionization and excitation of atmospheric constituents leading to auroral emissions was discovered in 1960, when a pioneering rocket flight from Fort Churchill in Canada revealed a flux of electrons entering the atmosphere from above.<ref>{{cite journal|last1=McIlwain|first1=C E|title=Direct Measurement of Particles Producing Visible Auroras|journal=Journal of Geophysical Research|year=1960|volume=65|issue=9|page=2727|doi=10.1029/JZ065i009p02727|bibcode=1960JGR....65.2727M}}</ref> Since then an extensive collection of measurements has been acquired painstakingly and with steadily improving resolution since the 1960s by many research teams using rockets and satellites to traverse the auroral zone. The main findings have been that auroral arcs and other bright forms are due to electrons that have been accelerated during the final few 10,000 km or so of their plunge into the atmosphere.<ref>{{Cite journal|doi=10.1029/JA093iA07p07441|title=Determination of auroral electrostatic potentials using high- and low-altitude particle distributions|journal=Journal of Geophysical Research|volume=93|issue=A7|page=7441|year=1988|last1=Reiff|first1=P. H.|last2=Collin|first2=H. L.|last3=Craven|first3=J. D.|last4=Burch|first4=J. L.|last5=Winningham|first5=J. D.|last6=Shelley|first6=E. G.|last7=Frank|first7=L. A.|last8=Friedman|first8=M. A.|bibcode=1988JGR....93.7441R }}</ref> These electrons often, but not always, exhibit a peak in their energy distribution, and are preferentially aligned along the local direction of the magnetic field. Electrons are mainly responsible for diffuse and pulsating auroras have, in contrast, a smoothly falling energy distribution, and an angular (pitch-angle) distribution favouring directions perpendicular to the local magnetic field. Pulsations were discovered to originate at or close to the equatorial crossing point of auroral zone magnetic field lines.<ref>{{Cite journal|doi=10.1038/215045a0|title=Evidence for Velocity Dispersion in Auroral Electrons|journal=Nature|volume=215|issue=5096|page=45|year=1967|last1=Bryant|first1=D. A.|last2=Collin|first2=H. L.|last3=Courtier|first3=G. M.|last4=Johnstone|first4=A. D.|bibcode=1967Natur.215...45B|s2cid=4173665 }}</ref> Protons are also associated with auroras, both discrete and diffuse.
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Aurora
(section)
Add topic