4.8 Article

Alfven Waves in the Lower Solar Atmosphere

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SCIENCE
卷 323, 期 5921, 页码 1582-1585

出版社

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1168680

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资金

  1. Northern Ireland Department for Employment and Learning [Studentship]
  2. NSF, Hungary [K67746]
  3. Atomic Weapons Establishment Aldermaston [William Penney Fellowship]
  4. Science and Technology Facilities Council
  5. STFC [ST/F002270/1, ST/H008799/1, ST/F002327/1, PP/E000711/1] Funding Source: UKRI
  6. Science and Technology Facilities Council [ST/F002270/1, PP/E000711/1, ST/H008799/1, ST/F002327/1] Funding Source: researchfish

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The flow of energy through the solar atmosphere and the heating of the Sun's outer regions are still not understood. Here, we report the detection of oscillatory phenomena associated with a large bright-point group that is 430,000 square kilometers in area and located near the solar disk center. Wavelet analysis reveals full-width half-maximum oscillations with periodicities ranging from 126 to 700 seconds originating above the bright point and significance levels exceeding 99%. These oscillations, 2.6 kilometers per second in amplitude, are coupled with chromospheric line-of-sight Doppler velocities with an average blue shift of 23 kilometers per second. A lack of cospatial intensity oscillations and transversal displacements rules out the presence of magneto-acoustic wave modes. The oscillations are a signature of Alfven waves produced by a torsional twist of +/- 22 degrees. A phase shift of 180 degrees across the diameter of the bright point suggests that these torsional Alfven oscillations are induced globally throughout the entire brightening. The energy flux associated with this wave mode is sufficient to heat the solar corona.

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