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Sound Waves from the Northern Lights. Jada Maxwell. Photo courtesy of Bjorn Jorgensen, 18 January 2005, near Tromsø, Norway http://www.spaceweather.com/aurora/images2005/17jan05/Jorgensen1.jpg. Coronal Mass Ejection (CME).
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Sound Waves from the Northern Lights Jada Maxwell Photo courtesy of Bjorn Jorgensen, 18 January 2005, near Tromsø, Norway http://www.spaceweather.com/aurora/images2005/17jan05/Jorgensen1.jpg
Coronal Mass Ejection (CME) Illustration by Steele Hill, courtesy of NASAhttp://sohowww.nascom.nasa.gov/localinfo/steele.html
Particles Spiral Down Field Lines Image: Fundamentals of Physics, 2005
Particles Spiral Down Field Lines Particles 2 • Collide with atomic and molecular oxygen and nitrogen • Emit energy as light
This Creates the Aurorae • Northern Lights = Aurora Borealis • Southern Lights = Aurora Australis Image courtesy of Shawn Malonehttp://www.lakesuperiorphoto.com
Can we hear the aurorae? • Anecdotal evidence of auroral sounds • hissing, popping, crackling, swooshing • corresponds with motions of light
6 minutes • Sound would take at least 6 minutes to travel from the aurora to the ground • No recordings of audible aurorae
Evidence of Infrasoundfrom Aurorae • Humans can hear between 20 and 20,000 Hertz (Hz) • Infrasound is below 20 Hz • Currently being investigated
The corona of the Sun is hotter than the surface! Image: Universe, 6th ed., 2002
Energy of Sound Waves is Transformed into Magnetic Waves Sun
Types of Magnetic Waves • Alfvén waves (s-mode) • Magnetosonic waves (p-mode) S-mode image courtesy of Georgia State Universityhttp://hyperphysics.phy-astr.gsu.edu/hbase/sound/tralon.html BBC animations
Magnetic Waves Earth
Beta is a Clue Gas Pressure Beta = β = Magnetic Field Pressure
Plasma is like… β = 1 is important
Mechanism for Transformation y (B0, k) y (B0) x (v1, B1) x (v1, B1, k) z (E1) z (E1) Alfvén waves Magnetosonic waves
Mechanism for Transformation y (B0, k) y (B0) v1 p v1 p x (v1, B1) x (v1, B1, k) E1 p E1 p z (E1) z (E1) Alfvén waves to Acoustic waves Magnetosonic waves to Acoustic waves
β= 1 in Earth’s atmosphere? When Beta = 1
What have we learned? MHD Waves ? observed CMEs Infrasound observed observed Aurorae
Future Plans • Gather data from satellite observations of resonant acoustic and Alfvén waves in a single CME induced geomagnetic event • Evaluate how wave velocities, frequencies and wavelengths change as altitude and β changes • Use data of auroral infrasound observed at Earth’s surface to extrapolate speeds in the ionosphere and compare to magnetic wave speeds
Image Sources: • NASAhttp://sohowww.nascom.nasa.gov/localinfo/steele.html • Shawn Malonehttp://www.lakesuperiorphoto.com • Halliday/Resnick/Walker. Fundamentals of Physics, John Wiley & Sons, 2005, p 746 Website: http://academic.evergreen.edu/m/maxjad02