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Title: The stability of the mesospheric plasma layer

Journal Article · · Physics of Plasmas
DOI:https://doi.org/10.1063/1.3671958· OSTI ID:22047137
 [1];  [2]
  1. Department of Physics, Macquarie University, Sydney, NSW 2109 (Australia)
  2. School of Physics, University of Sydney, NSW 2006 (Australia)

The presence of micron and sub-micron size dust in the Earth's summer mesopause are a possible cause of electron density depletion. Whereas electrons in this weakly ionized and weakly magnetized layer are frozen in the magnetic field, the ions and dust are highly diffusive. This relative drift between the plasma particles will cause a current in the medium. The presence of such a current can destabilize the plasma layer with a growth rate of the order of Alfven frequency. Since required current density for the onset of this instability is on the order of J > or approx. 0.03A/m{sup 2}, it is quite unlikely that such a strong current is present in the mesosphere. However, owing to the prevailing ambiguity of measurements, the existence of such a current is not completely ruled out.

OSTI ID:
22047137
Journal Information:
Physics of Plasmas, Vol. 18, Issue 12; Other Information: (c) 2011 American Institute of Physics; Country of input: International Atomic Energy Agency (IAEA); ISSN 1070-664X
Country of Publication:
United States
Language:
English