Physics
Scientific paper
Aug 1990
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990jatp...52..637h&link_type=abstract
(EISCAT Scientific Association, International EISCAT Workshop, 4th, Sigtuna, Sweden, June 5-9, 1989) Journal of Atmospheric and
Physics
89
Dust, Ionospheric Electron Density, Mesopause, Radar Scattering, Summer, Ice, Incoherent Scatter Radar, Noctilucent Clouds, Optical Thickness
Scientific paper
It is proposed that dust formed at the cool summer mesopause may have optical properties very different from that measured for bulk material of ice. The smallness of the dust and possible surface impurities may lead to high photoelectric yields and low work functions. For such reasons the dust in the summer mesopause may, at least occasionally, be charged to substantial positive surface potentials while pure ice, with its high photoelectric workfunction, would be charged to low and negative potentials by collisions with plasma particles. The presence of 'dressed' dust particles, with surface potentials of some volts, can lead to enhanced radar backscatter. The dust density which is required by the present model to explain radar backscatter and electron bite-outs is of the order of 10/cu cm for dust of radius above 5 x 10 to the -6th cm.
Bingham Richard
de Angelis Umberto
Goertz Christoph K.
Havnes Ove
Morfill Gregor E.
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