Earth's Magnetic Song Recorded For The First Time During A Solar Storm

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  1. CULCULCAN

    CULCULCAN The Final Synthesis - isbn 978-0-9939480-0-8 Staff Member

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    Earth's magnetic song

    recorded for the first time

    during a solar storm


    November 19, 2019 , European Space Agency
    1-earthsmagnet.
    In this image, Earth is the dot to the left of the image and the large arc around it is our planet’s magnetic bow shock. The swirling pattern to the right is the foreshock region where the solar wind breaks into waves as it encounters reflected particles from the bow shock. The image was created using the Vlasiator model, a computer simulation developed at the University of Helsinki to study Earth’s magnetic interaction with the solar wind. Credit: Vlasiator team, University of Helsinki
    Data from ESA's Cluster mission has provided
    a recording of the eerie "song" that Earth sings
    when it is hit by a solar storm.
    The song comes from waves that are generated in the Earth's
    magnetic field by the collision of the storm.

    The storm itself is the eruption of electrically charged particles
    from the sun's atmosphere.

    A team led by Lucile Turc, a former ESA research fellow
    who is now based at the University of Helsinki, Finland,
    made the discovery after analyzing data
    from the Cluster Science Archive.

    The archive provides access to all data obtained
    during Cluster's ongoing mission over almost two decades.

    Cluster consists of four spacecraft that orbit Earth in formation,
    investigating our planet's magnetic environment and its interaction
    with the solar wind—a constant flow of particles released
    by the sun into the Solar System.

    As part of their orbits, the Cluster spacecraft repeatedly
    fly through the foreshock, which is the first region
    that particles encounter when a solar storm hits our planet.

    The team found that in the early part of the mission,
    from 2001 to 2005, the spacecraft flew through six such collisions,
    recording the waves that were generated.

    The new analysis shows that, during the collision,
    the foreshock is driven to release magnetic waves
    that are much more complex than first thought.
    The magnetic waves measured by ESA’s Cluster mission in the magnetic foreshock above Earth – the first region of our planet’s magnetic environment that solar wind particles encounter – during calm space weather conditions. The video contains a ‘sonification’ of the magnetic waves in the undisturbed foreshock, obtained by transforming the frequencies of these magnetic waves into audible signals. In the undisturbed foreshock, the sounds are very low pitch and monotonous. Credit: ESA/Cluster; L. Turc et al. (2019); Audio: Martin Archer, Queen Mary University of London, CC BY-SA 3.0 IGO
    "Our study reveals that solar storms profoundly modify
    the foreshock region," says Lucile.

    When the frequencies of these magnetic waves
    are transformed into audible signals,
    they give rise to an uncanny song that might recall
    more the sound effects of a science fiction movie
    than a natural phenomenon.

    In quiet times, when no solar storm is striking the Earth,
    the song is lower in pitch and less complex,
    with one single frequency dominating the oscillation.

    When a solar storm hits, the frequency of the wave
    is roughly doubled, with the precise frequency
    of the resulting waves being dependent
    on the strength of the magnetic field in the storm.
    "It's like the storm is changing the tuning of the foreshock,"
    explains Lucile.

    And it doesn't stop there because not only does the frequency
    of the wave change but it also becomes much more complicated
    than the single frequency present in quiet times.

    Once the storm hits the foreshock, the wave breaks
    into a complex network of different, higher frequencies.

    Computer simulations of the foreshock, performed
    using a model called Vlasiator, which is being developed
    at the University of Helsinki, demonstrate the intricate
    wave pattern that appears during solar storms.
    The magnetic waves measured by ESA’s Cluster mission in the magnetic foreshock above Earth – the first region of our planet’s magnetic environment that solar wind particles encounter
    – during a solar storm.
    The video contains a ‘sonification’ of the magnetic waves obtained by transforming the frequencies of these magnetic waves into audible signals. During the storm, the magnetic waves in the foreshock roughly double their frequency and become more complicated than during calm space weather conditions, resulting in audible sounds that are around an octave higher and much more variable.
    Credit: ESA/Cluster; L. Turc et al. (2019); Audio: Martin Archer, Queen Mary University of London, CC BY-SA 3.0 IGO
    The changes in the foreshock have the power to affect the way
    the solar storm is propagated down to the Earth's surface.

    Although it is still an open question exactly how this process works,
    it is clear that the energy generated by waves in the foreshock
    cannot escape back into space, as the waves are pushed
    towards Earth by the incoming solar storm.

    Before they reach our atmosphere, however, the waves encounter
    another barrier, the bow shock, which is the magnetic region
    of space that slows down solar wind particles before they collide
    with Earth's magnetic field.

    The collision of the magnetic waves modifies
    the behaviour of the bow shock,
    possibly changing the way it processes the energy
    of the incoming solar storm.

    Behind the bow shock, the magnetic fields of Earth
    start to resonate at the frequency of the waves
    and this contributes to transmit the magnetic disturbance
    all the way to the ground.

    It is a fast process, taking around ten minutes
    from the wave being generated at the foreshock
    to its energy reaching the ground.

    Lucile and colleagues are now working to understand
    exactly how these complex waves are generated.

    "We always expected a change in frequency
    but not the level of complexity in the wave," she adds.

    Solar storms are a part of space weather.

    While the solar wind is always blowing,
    explosive releases of energy close to the sun's surface
    generate turbulence and gusts that eventually give rise
    to solar storms.
    This movie from the Vlasiator computer model shows the foreshock above Earth – the first region of our planet’s magnetic environment that solar wind particles encounter – being engulfed by a magnetic cloud
    during a solar storm. The waves generally become much smaller,
    and so higher in frequency, than those arising
    during calm space weather conditions,
    and they break up into a much more complicated pattern,
    which contains many different frequencies.
    Credit: Vlasiator team, University of Helsinki
    Understanding space weather has become increasingly important
    to society because of the damaging effects solar storms
    can have on sensitive electronics and technology
    on ground and in space.

    It is now more important than ever that we understand how space weather disturbances such as solar storms propagate through the Solar System
    and down to Earth, and ESA's upcoming Solar Orbiter mission,
    scheduled for launch in February 2020,
    will greatly contribute to these investigations.

    This new scientific study based on the long-lived Cluster mission
    provides another detail in that knowledge but it also has a larger role
    to play in our understanding of the universe.

    Magnetic fields are ubiquitous and so the kind of complex interaction
    seen in Earth's foreshock may take place in a variety
    of cosmic environments, including exoplanets orbiting
    close to their parent star, as they would be immersed
    in intense magnetic fields.

    "This is an excellent example of how Cluster continues
    to extend our knowledge of the sun-Earth connection,
    even years after the original data was obtained,"
    says Philippe Escoubet, ESA Project Scientist for Cluster.

    "The results take us deeper into the details
    of fundamental magnetic interactions
    that take place across the universe."
    More information: L. Turc et al. First observations
    of the disruption of the Earth's foreshock wave field during magnetic clouds, Geophysical Research Letters. DOI: 10.1029/2019GL084437

    The audio files with the sonification of the Cluster measurements
    are available on ESA's Soundcloud page: soundcloud.com/esa

    Journal information: Geophysical Research Letters

    Provided by European Space Agency

    https://m.phys.org/news/2019-11-ear...RDX_r-3T7zmlhGIFLR5Lh4wArHxe7cmg3HSrEN1mZARs0
     

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