The
first observation of mode conversion of whistler waves to
lower hybrid waves at a density striation has been made
in a laboratory plasma. The observed lower hybrid wavelength
is consistent with that predicted by linear mode coupling.
The lower hybrid waves have amplitudes up to 20% of the
incident whistler waves.
Whistler
waves are launched toward a field-aligned density striation
in a laboratory plasma. Characteristic scale length and frequency
ratios are scaled so as to closely reproduce situations found
in the auroral ionosphere. Detailed measurements show that
at the striation edge nearest the wave-launching antenna,
besides a reflected and a transmitted whistler wave, lower
hybrid waves are also stimulated on both sides of the striation
boundary in a manner consistent with the linear mode-conversion
model. We find that the energy density of the mode-converted
lower hybrid waves is almost 20% of the incident whistler
wave energy density. The interaction takes place wherever
the incident wave vector has a component perpendicular to
the striation surface. Lower hybrid waves are confined to
within 2-3 perpendicular wavelengths in the interaction zone.
Our results show that the interaction of electromagnetic whistler
mode waves with density striations can cause significant amounts
of energy to be deposited in the largely electrostatic lower
hybrid mode and that it may, therefore, be a significant generation
mechanism for these waves in certain regions of the ionosphere.