University of Crete Island of Crete

Meteor Science and Layering Phenomena in the Lower Thermosphere.
Is there anything that we lack in basic knowledge and how should we go about getting it?

J. D. Mathews

The Pennsylvania State University, University Park, PA, USA

The micrometeoroid mass flux into the upper atmosphere has long been recognized as providing the atomic metal ions necessary to the formation of sporadic-E and lidar-visible metal layers. While this mass flux as a function of local time, season, and latitude remains very much an issue, recent VHF and UHF HPLA (High-Power, Large Aperture) radar meteor head-echo observations have provided estimates of this flux using direct radial or 3-D Doppler and deceleration measurements that yield good particle mass estimates under reasonable assumptions. These observations have shown that the micrometeoroid speed distribution is much higher than previously assumed and that the well know visible meteor showers contribute little mass to the upper atmosphere relative to the daily sporadic meteoroid flux. Other issues now being addressed with HPLA radars include details of the meteoroid interaction with atmosphere and the related radio science and plasma physics issues that must be resolved in order to understand what the radar actually “sees”. In particular, we now recognize that the meteoroid interaction with the atmosphere is anything but simple with meteoroids undergoing fragmentation and terminal (explosive) events thus complicating observations and pointing to a significant mass flux component in nanometer particle form rather than atom-level ablation products. Observations of long-lived range-spread (meteor) trail-echoes (RSTEs) have led to the understanding that these events are caused by the rapid alignment of the meteor trails along the geomagnetic field yielding FAI-scattering. RSTE observations then enable the study of the plasma processes including diffusion and electrodynamic instabilities that drive the trail-plasma to B-field align. These studies also cast new light on the diffusion rates determined using “classical” meteor radar observations of decaying trail-echoes and on the formation of altitude-narrow ion layers. We note that multi-frequency, common-volume radar meteor observations will prove especially useful in resolving the issues raised.

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