Loading…

Coherent large beamwidth processing of radio-echo sounding data

Coherent processing of radio-echo sounding data of polar ice sheets is known to provide an indication of bedrock properties and detection of internal layers. We investigate the benefits of coherent processing of a large azimuth beamwidth to retrieve and characterize the orientation and angular backs...

Full description

Saved in:
Bibliographic Details
Published in:The cryosphere 2018-09, Vol.12 (9), p.2969-2979
Main Authors: Heister, Anton, Scheiber, Rolf
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3
cites cdi_FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3
container_end_page 2979
container_issue 9
container_start_page 2969
container_title The cryosphere
container_volume 12
creator Heister, Anton
Scheiber, Rolf
description Coherent processing of radio-echo sounding data of polar ice sheets is known to provide an indication of bedrock properties and detection of internal layers. We investigate the benefits of coherent processing of a large azimuth beamwidth to retrieve and characterize the orientation and angular backscattering properties of the surface and subsurface features. MCRDS data acquired over two distinct test areas in Greenland are used to demonstrate the specular backscattering properties of the ice surface and of the internal layers, as well as the much wider angular response of the bedrock. The coupling of internal layers' orientation with the bed topography is shown to increase with depth. Spectral filtering can be used to increase the SNR of the internal layers and mitigate the surface multiple. The variance of the bed backscattering can be used to characterize the bed return specularity. The use of the SAR-focused RES data ensures the correct azimuth positioning of the internal layers for the subsequent slope estimation.
doi_str_mv 10.5194/tc-12-2969-2018
format article
fullrecord <record><control><sourceid>gale_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_bad0cdd8e43a4938b6a0d755b7d68055</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A554853674</galeid><doaj_id>oai_doaj_org_article_bad0cdd8e43a4938b6a0d755b7d68055</doaj_id><sourcerecordid>A554853674</sourcerecordid><originalsourceid>FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3</originalsourceid><addsrcrecordid>eNptkUtLJDEUhYthBkYd124LXLkozbuS1SCNjwZBmMc63MqjOk13xUnSqP_etC1qwxAuCYfvntzLaZoTjM45VuyimA6TjiihOoKw_NIcYKVYhxhhXz-9vzeHOS8REkQhdtD8nMWFS24q7QrS6NrBwfox2LJoH1I0LucwjW30bQIbYufMIrY5bia7lS0U-NF887DK7vjtPmr-Xl_9md12d_c389nlXQccodIRipWnnPtBKsUZ58oLX0uo3ljHevDMChgq0pOeYSKkw96D8VwgSamhR81852sjLPVDCmtIzzpC0K9CTKOGVIJZOT2ARcZa6RgFpqgcBCDbcz70VkjEefU63XnVFf9tXC56GTdpquNrgpGUpH4vPqgRqmmYfCwJzDpkoy85Z5JT0bNKnf-Hqse6dTBxcj5Ufa_hbK-hMsU9lRE2Oev571_77MWONSnmnJx_XxwjvQ1dF6Mx0dvQ9TZ0-gKewpvY</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2108822686</pqid></control><display><type>article</type><title>Coherent large beamwidth processing of radio-echo sounding data</title><source>Publicly Available Content Database</source><creator>Heister, Anton ; Scheiber, Rolf</creator><creatorcontrib>Heister, Anton ; Scheiber, Rolf</creatorcontrib><description>Coherent processing of radio-echo sounding data of polar ice sheets is known to provide an indication of bedrock properties and detection of internal layers. We investigate the benefits of coherent processing of a large azimuth beamwidth to retrieve and characterize the orientation and angular backscattering properties of the surface and subsurface features. MCRDS data acquired over two distinct test areas in Greenland are used to demonstrate the specular backscattering properties of the ice surface and of the internal layers, as well as the much wider angular response of the bedrock. The coupling of internal layers' orientation with the bed topography is shown to increase with depth. Spectral filtering can be used to increase the SNR of the internal layers and mitigate the surface multiple. The variance of the bed backscattering can be used to characterize the bed return specularity. The use of the SAR-focused RES data ensures the correct azimuth positioning of the internal layers for the subsequent slope estimation.</description><identifier>ISSN: 1994-0424</identifier><identifier>ISSN: 1994-0416</identifier><identifier>EISSN: 1994-0424</identifier><identifier>EISSN: 1994-0416</identifier><identifier>DOI: 10.5194/tc-12-2969-2018</identifier><language>eng</language><publisher>Katlenburg-Lindau: Copernicus GmbH</publisher><subject>Azimuth ; Backscatter ; Backscattering ; Bedrock ; Coherence ; Data ; Data acquisition ; Data processing ; Detection ; Echo sounding ; Echoes ; Filtration ; Geophysical research ; Glaciation ; Ice ; Ice sheets ; Observations ; Orientation ; Properties ; Properties (attributes) ; Radio ; SAR (radar) ; Topography (geology)</subject><ispartof>The cryosphere, 2018-09, Vol.12 (9), p.2969-2979</ispartof><rights>COPYRIGHT 2018 Copernicus GmbH</rights><rights>2018. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3</citedby><cites>FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2108822686/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2108822686?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,25731,27901,27902,36989,44566,74869</link.rule.ids></links><search><creatorcontrib>Heister, Anton</creatorcontrib><creatorcontrib>Scheiber, Rolf</creatorcontrib><title>Coherent large beamwidth processing of radio-echo sounding data</title><title>The cryosphere</title><description>Coherent processing of radio-echo sounding data of polar ice sheets is known to provide an indication of bedrock properties and detection of internal layers. We investigate the benefits of coherent processing of a large azimuth beamwidth to retrieve and characterize the orientation and angular backscattering properties of the surface and subsurface features. MCRDS data acquired over two distinct test areas in Greenland are used to demonstrate the specular backscattering properties of the ice surface and of the internal layers, as well as the much wider angular response of the bedrock. The coupling of internal layers' orientation with the bed topography is shown to increase with depth. Spectral filtering can be used to increase the SNR of the internal layers and mitigate the surface multiple. The variance of the bed backscattering can be used to characterize the bed return specularity. The use of the SAR-focused RES data ensures the correct azimuth positioning of the internal layers for the subsequent slope estimation.</description><subject>Azimuth</subject><subject>Backscatter</subject><subject>Backscattering</subject><subject>Bedrock</subject><subject>Coherence</subject><subject>Data</subject><subject>Data acquisition</subject><subject>Data processing</subject><subject>Detection</subject><subject>Echo sounding</subject><subject>Echoes</subject><subject>Filtration</subject><subject>Geophysical research</subject><subject>Glaciation</subject><subject>Ice</subject><subject>Ice sheets</subject><subject>Observations</subject><subject>Orientation</subject><subject>Properties</subject><subject>Properties (attributes)</subject><subject>Radio</subject><subject>SAR (radar)</subject><subject>Topography (geology)</subject><issn>1994-0424</issn><issn>1994-0416</issn><issn>1994-0424</issn><issn>1994-0416</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNptkUtLJDEUhYthBkYd124LXLkozbuS1SCNjwZBmMc63MqjOk13xUnSqP_etC1qwxAuCYfvntzLaZoTjM45VuyimA6TjiihOoKw_NIcYKVYhxhhXz-9vzeHOS8REkQhdtD8nMWFS24q7QrS6NrBwfox2LJoH1I0LucwjW30bQIbYufMIrY5bia7lS0U-NF887DK7vjtPmr-Xl_9md12d_c389nlXQccodIRipWnnPtBKsUZ58oLX0uo3ljHevDMChgq0pOeYSKkw96D8VwgSamhR81852sjLPVDCmtIzzpC0K9CTKOGVIJZOT2ARcZa6RgFpqgcBCDbcz70VkjEefU63XnVFf9tXC56GTdpquNrgpGUpH4vPqgRqmmYfCwJzDpkoy85Z5JT0bNKnf-Hqse6dTBxcj5Ufa_hbK-hMsU9lRE2Oev571_77MWONSnmnJx_XxwjvQ1dF6Mx0dvQ9TZ0-gKewpvY</recordid><startdate>20180919</startdate><enddate>20180919</enddate><creator>Heister, Anton</creator><creator>Scheiber, Rolf</creator><general>Copernicus GmbH</general><general>Copernicus Publications</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>7QH</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BFMQW</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope><scope>DOA</scope></search><sort><creationdate>20180919</creationdate><title>Coherent large beamwidth processing of radio-echo sounding data</title><author>Heister, Anton ; Scheiber, Rolf</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Azimuth</topic><topic>Backscatter</topic><topic>Backscattering</topic><topic>Bedrock</topic><topic>Coherence</topic><topic>Data</topic><topic>Data acquisition</topic><topic>Data processing</topic><topic>Detection</topic><topic>Echo sounding</topic><topic>Echoes</topic><topic>Filtration</topic><topic>Geophysical research</topic><topic>Glaciation</topic><topic>Ice</topic><topic>Ice sheets</topic><topic>Observations</topic><topic>Orientation</topic><topic>Properties</topic><topic>Properties (attributes)</topic><topic>Radio</topic><topic>SAR (radar)</topic><topic>Topography (geology)</topic><toplevel>online_resources</toplevel><creatorcontrib>Heister, Anton</creatorcontrib><creatorcontrib>Scheiber, Rolf</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>Aqualine</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Continental Europe Database</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>The cryosphere</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Heister, Anton</au><au>Scheiber, Rolf</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coherent large beamwidth processing of radio-echo sounding data</atitle><jtitle>The cryosphere</jtitle><date>2018-09-19</date><risdate>2018</risdate><volume>12</volume><issue>9</issue><spage>2969</spage><epage>2979</epage><pages>2969-2979</pages><issn>1994-0424</issn><issn>1994-0416</issn><eissn>1994-0424</eissn><eissn>1994-0416</eissn><abstract>Coherent processing of radio-echo sounding data of polar ice sheets is known to provide an indication of bedrock properties and detection of internal layers. We investigate the benefits of coherent processing of a large azimuth beamwidth to retrieve and characterize the orientation and angular backscattering properties of the surface and subsurface features. MCRDS data acquired over two distinct test areas in Greenland are used to demonstrate the specular backscattering properties of the ice surface and of the internal layers, as well as the much wider angular response of the bedrock. The coupling of internal layers' orientation with the bed topography is shown to increase with depth. Spectral filtering can be used to increase the SNR of the internal layers and mitigate the surface multiple. The variance of the bed backscattering can be used to characterize the bed return specularity. The use of the SAR-focused RES data ensures the correct azimuth positioning of the internal layers for the subsequent slope estimation.</abstract><cop>Katlenburg-Lindau</cop><pub>Copernicus GmbH</pub><doi>10.5194/tc-12-2969-2018</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1994-0424
ispartof The cryosphere, 2018-09, Vol.12 (9), p.2969-2979
issn 1994-0424
1994-0416
1994-0424
1994-0416
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_bad0cdd8e43a4938b6a0d755b7d68055
source Publicly Available Content Database
subjects Azimuth
Backscatter
Backscattering
Bedrock
Coherence
Data
Data acquisition
Data processing
Detection
Echo sounding
Echoes
Filtration
Geophysical research
Glaciation
Ice
Ice sheets
Observations
Orientation
Properties
Properties (attributes)
Radio
SAR (radar)
Topography (geology)
title Coherent large beamwidth processing of radio-echo sounding data
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-30T23%3A12%3A26IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Coherent%20large%20beamwidth%20processing%20of%20radio-echo%20sounding%20data&rft.jtitle=The%20cryosphere&rft.au=Heister,%20Anton&rft.date=2018-09-19&rft.volume=12&rft.issue=9&rft.spage=2969&rft.epage=2979&rft.pages=2969-2979&rft.issn=1994-0424&rft.eissn=1994-0424&rft_id=info:doi/10.5194/tc-12-2969-2018&rft_dat=%3Cgale_doaj_%3EA554853674%3C/gale_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a500t-2319f355fb89954559f6f9f6697cde47af4d6abf3572741268e1ffacf560833c3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2108822686&rft_id=info:pmid/&rft_galeid=A554853674&rfr_iscdi=true