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			<titleStmt><title level='a'>NSF COLDEX/Open Polar Radar Example Delay Doppler Classification of Englacial Reflectors</title></titleStmt>
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				<publisher>Texas Data Repository</publisher>
				<date>01/01/2025</date>
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				<bibl> 
					<idno type="par_id">10607883</idno>
					<idno type="doi">10.18738/T8/DM10IG</idno>
					
					<author>Duncan Young</author><author>Gregory Ng</author><author>Scott D Kempf</author><author>Duncan Young</author>
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			<abstract><ab><![CDATA[&lt;p&gt;This is an example line of NSF COLDEX MARFA ice penetrating radar data(CLX/MKB2o/R66a) that has been processed to provide azimuthal information about radar echos from below, and to the front and back of the aircraft. The input was 1 meter slow time resampled coherent range record with phase intact. The data were pulse compressed and an azimuth fast Fourier transform was used to convert to azimuth angles in 1 km chunks, then slices at -19°, &#43;19˚ and nadir were selected for these numpy arrays. These can be displayed as an RGB image with Blue &#61; nadir, red &#61; forward and green &#61; rear&lt;/p&gt;&lt;p&gt;The nadir slice should dominate specular echos, as seen with englacial reflecting horizons; where this trades to more balanced returns across all three channels, scattering dominates, as with rough bed rock or volume scattering. A gmt text file contains information about where this transition occurs in the ice column.&lt;/p&gt;&lt;p&gt;Details in delay Doppler processing can be found in &lt;a href&#61;&#34;http://pds-geosciences.wustl.edu/mro/mro-m-sharad-5-radargram-v1/mrosh_2001/document/rgram_processing.pdf&#34;&gt;Campbell et al., 2014&lt;/a&gt;; the idea for using this approach for looking at englacial structure was discussed by &lt;a href&#61;&#34;https://doi.org/10.5194/egusphere-egu23-2856&#34;&gt;Arenas-Pingarrón, Á. et al.,2023&lt;/a&gt;. Details of HiCARs/MARFA focused processing can be found in &lt;a href&#61;&#34;http://dx.doi.org/10.1109/TGRS.2007.897416&#34;&gt;Peters et al., 2007&lt;/a&gt;.&lt;/p&gt;]]></ab></abstract>
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