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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>4</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-695-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/695/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/695/2004/acpd-4-695-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/695/2004/acpd-4-695-2004.pdf</fulltext_pdf>
	<start_page>695</start_page>
	<end_page>729</end_page>
	<publication_date>2004-02-02</publication_date>
	<article_title content_type="html">Radar observations of meteor trails, and their interpretation using Fresnel holography: a new tool in meteor science</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. G. Elford</name>
			<email>wgelford@aol.com</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physics and Mathematical Physics, University of Adelaide, Adelaide, 5005, Australia</affiliation>
	</affiliations>
	<abstract content_type="html">A Fresnel Transform technique has been developed at Adelaide to analyse
      radar meteor echoes detected in the transverse mode. The genesis for this technique was the study of the structure of the scattering ionization
      immediately behind the head of the trail, in order to deduce the degree of
      fragmentation of the ablating meteoroid. The technique has been remarkably
      successful in not only giving insight into the fragmentation of meteoroids,
      but also revealing other significant features of the trails including diffusion, lateral motion of the trail during formation due to wind drift,
      and phase of the scattered signal in the vicinity of the head of the trail.&lt;br&gt;
      &lt;br&gt;
      A serendipitous outcome of the analysis is the measurement of the speed and
      deceleration of the meteoroid producing the trail to a precision far exceeding that available from any other method applied to transverse scatter
      data.&lt;br&gt;
      &lt;br&gt;
      Examples of the outcomes of the technique applied to meteor echoes obtained
      with a 54 MHz narrow beam radar are presented.</abstract>
	<references>
	</references>
</article>

