@InProceedings{MuralikrishnaKulk:2009:RoMeDu,
author = "Muralikrishna, Polinaya and Kulkarni, V. H.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {University
of Bombay}",
title = "Role of meteoric dust in the e-region dynamics",
booktitle = "Proceedings...",
year = "2009",
organization = "Iaga, 2009.",
keywords = "Meteoric Dust, E-region dynamics, Electrical conductivity,
Collision frequency.",
abstract = "Dust particles play an important role in the dynamics of the
E-region. Ablation of meteors that enter the atmosphere with
velocities ¡{\"O}15 kms-1 is the most important source of these
dust particles of micron and submicron sizes. Polar Mesospheric
Summer Echoes in the polar region and the blanketing sporadic-E
layers in the low latitude E-region are known to be manifestations
of dust particles. Large amounts of dust particles with average
sizes of about 0.1¦{\`{\I}} with number densities of up to
several thousands per cubic centimeter and charge densities of the
same order were detected experimentally. In some parts of the dust
layers it was found that the negative charge density on dusts was
so large that the number of free electrons was significantly
reduced there, since the dust acted as a sink for electrons, thus
causing electron bite outs. Recent studies show the possible role
of neutral as well as charged dust particles of submicron size in
altering the conductivity parameters in the equatorial E-region
through the collision frequencies. In the upper E-region the dust
particles are not very effective in capturing the ambient
electrons and so do not affect the quase neutrality of the plasma.
But they can alter the effective collision frequencies of the
ambient electrons in this region by a factor as high as 4. They
can also reduce significantly the growth rate and amplitude of
plasma irregularities in this region. In the lower E-region the
dust particles get charged by capturing the ambient electrons and
affect significantly the electrical conductivities. When exist in
sufficient numbers, charged dust particles can even reverse the
ambient vertical polarization electric field in the lower E-region
altitudes. Assuming a simple exponential model for the dust layer,
the role of these dust particles in altering the E-region dynamics
by affecting the collision and conductivity parameters is
investigated here.",
conference-location = "Sopron, Hungary",
conference-year = "23-30 Aug.",
language = "en",
urlaccessdate = "10 maio 2024"
}