Upward-looking L-band FMCW radar for snow cover monitoring

Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk a...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Cold regions science and technology 2014-07, Vol.103 (100), p.31-40
Hauptverfasser: Okorn, Robert, Brunnhofer, Georg, Platzer, Thomas, Heilig, Achim, Schmid, Lino, Mitterer, Christoph, Schweizer, Jürg, Eisen, Olaf
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 40
container_issue 100
container_start_page 31
container_title Cold regions science and technology
container_volume 103
creator Okorn, Robert
Brunnhofer, Georg
Platzer, Thomas
Heilig, Achim
Schmid, Lino
Mitterer, Christoph
Schweizer, Jürg
Eisen, Olaf
description Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk assessment. We present a low-cost L-band frequency modulated continuous wave radar system (FMCW) in upward-looking configuration. To monitor the snowpack evolution, the radar system was deployed in fall and subsequently was covered by snowfalls. During two winter seasons we recorded reflections from the overlying snowpack. The influence of reflection magnitude and phase to the measured frequency spectra, as well as the influence of signal processing were investigated. We present a method to extract the phase of the reflection coefficients from the phase response of the frequency spectra and their integration into the presentation of the measurement data. The phase information significantly improved the detectability of the temporal evolution of the snow surface reflection. We developed an automated and a semi-automated snow surface tracking algorithm. Results were compared with independently measured snow height from a laser snow-depth sensor and results derived from an upward-looking impulse radar system (upGPR). The semi-automated tracking used the phase information and had an accuracy of about 6 to 8cm for dry-snow conditions, similar to the accuracy of the upGPR, compared to measurements from the laser snow-depth sensor. The percolation of water was observable in the radargrams. Results suggest that the upward-looking FMCW system may be a valuable alternative to conventional snow-depth sensors for locations, where fixed installations above ground are not feasible. •Snowpack measurement with upward-looking FMCW radar•Method to extract the phase of the reflection coefficients•Include phase into the illustration of the measurement data•Automated and semi-automated snow surface tracking algorithm•Improved snow surface tracking when using the phase of the reflection coefficients
doi_str_mv 10.1016/j.coldregions.2014.03.006
format Article
fullrecord <record><control><sourceid>proquest_pubme</sourceid><recordid>TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4045589</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0165232X14000615</els_id><sourcerecordid>1776653727</sourcerecordid><originalsourceid>FETCH-LOGICAL-c579t-8c0e23197cb01aaf0e380f7a32f2ecc3f020110fb9bc3fd32b31581d89239cab3</originalsourceid><addsrcrecordid>eNqNkU2LFDEQhoMo7rj6F6Q9CF66rXx0J_EgyOCqMOLFRW8hnY8xY08yJj2z-O_NMOO6nvRUFPXUSxUPQs8wdBjw8HLTmTTZ7NYhxdIRwKwD2gEM99ACC05azhi-jxaV7VtCydcL9KiUDdRe9vQhuiBMSiYZXaBX17sbnW07pfQ9xHWzakcdbXP1cfmlydrq3PiUmxLTTWPSweVmm2KYU67sY_TA66m4J-d6ia6v3n5evm9Xn959WL5Ztabncm6FAUcoltyMgLX24KgAzzUlnjhjqIf6AAY_yrE2lpKR4l5gKySh0uiRXqLXp9zdftw6a1ycs57ULoetzj9V0kH9PYnhm1qng2LA-l7IGvDiHJDTj70rs9qGYtw06ejSvigsABjHYuD_Rjkfhp5yckTlCTU5lZKdv70IgzpqUht1R5M6alJAVdVUd5_efel287eXCjw_A7oYPfmsownlDycY7wWwyi1PnKsCDsFlVUxw0TgbsjOzsin8xzm_ADa-tuw</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1776653727</pqid></control><display><type>article</type><title>Upward-looking L-band FMCW radar for snow cover monitoring</title><source>Access via ScienceDirect (Elsevier)</source><creator>Okorn, Robert ; Brunnhofer, Georg ; Platzer, Thomas ; Heilig, Achim ; Schmid, Lino ; Mitterer, Christoph ; Schweizer, Jürg ; Eisen, Olaf</creator><creatorcontrib>Okorn, Robert ; Brunnhofer, Georg ; Platzer, Thomas ; Heilig, Achim ; Schmid, Lino ; Mitterer, Christoph ; Schweizer, Jürg ; Eisen, Olaf</creatorcontrib><description>Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk assessment. We present a low-cost L-band frequency modulated continuous wave radar system (FMCW) in upward-looking configuration. To monitor the snowpack evolution, the radar system was deployed in fall and subsequently was covered by snowfalls. During two winter seasons we recorded reflections from the overlying snowpack. The influence of reflection magnitude and phase to the measured frequency spectra, as well as the influence of signal processing were investigated. We present a method to extract the phase of the reflection coefficients from the phase response of the frequency spectra and their integration into the presentation of the measurement data. The phase information significantly improved the detectability of the temporal evolution of the snow surface reflection. We developed an automated and a semi-automated snow surface tracking algorithm. Results were compared with independently measured snow height from a laser snow-depth sensor and results derived from an upward-looking impulse radar system (upGPR). The semi-automated tracking used the phase information and had an accuracy of about 6 to 8cm for dry-snow conditions, similar to the accuracy of the upGPR, compared to measurements from the laser snow-depth sensor. The percolation of water was observable in the radargrams. Results suggest that the upward-looking FMCW system may be a valuable alternative to conventional snow-depth sensors for locations, where fixed installations above ground are not feasible. •Snowpack measurement with upward-looking FMCW radar•Method to extract the phase of the reflection coefficients•Include phase into the illustration of the measurement data•Automated and semi-automated snow surface tracking algorithm•Improved snow surface tracking when using the phase of the reflection coefficients</description><identifier>ISSN: 0165-232X</identifier><identifier>EISSN: 1872-7441</identifier><identifier>DOI: 10.1016/j.coldregions.2014.03.006</identifier><identifier>PMID: 24994943</identifier><identifier>CODEN: CRSTDL</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Earth, ocean, space ; Exact sciences and technology ; External geophysics ; FMCW ; Geophysics. Techniques, methods, instrumentation and models ; Lasers ; Radar ; Reflection ; Sensors ; Snow ; Snow avalanches ; Snow stratigraphy ; Snow. Ice. Glaciers ; Snowpack ; Snowpack monitoring ; Surface tracking ; Tracking</subject><ispartof>Cold regions science and technology, 2014-07, Vol.103 (100), p.31-40</ispartof><rights>2014 The Authors</rights><rights>2015 INIST-CNRS</rights><rights>2014 The Authors 2014</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c579t-8c0e23197cb01aaf0e380f7a32f2ecc3f020110fb9bc3fd32b31581d89239cab3</citedby><cites>FETCH-LOGICAL-c579t-8c0e23197cb01aaf0e380f7a32f2ecc3f020110fb9bc3fd32b31581d89239cab3</cites><orcidid>0000-0001-5076-2968 ; 0000-0001-9826-4191</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.coldregions.2014.03.006$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,885,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=28475804$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/24994943$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Okorn, Robert</creatorcontrib><creatorcontrib>Brunnhofer, Georg</creatorcontrib><creatorcontrib>Platzer, Thomas</creatorcontrib><creatorcontrib>Heilig, Achim</creatorcontrib><creatorcontrib>Schmid, Lino</creatorcontrib><creatorcontrib>Mitterer, Christoph</creatorcontrib><creatorcontrib>Schweizer, Jürg</creatorcontrib><creatorcontrib>Eisen, Olaf</creatorcontrib><title>Upward-looking L-band FMCW radar for snow cover monitoring</title><title>Cold regions science and technology</title><addtitle>Cold Reg Sci Technol</addtitle><description>Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk assessment. We present a low-cost L-band frequency modulated continuous wave radar system (FMCW) in upward-looking configuration. To monitor the snowpack evolution, the radar system was deployed in fall and subsequently was covered by snowfalls. During two winter seasons we recorded reflections from the overlying snowpack. The influence of reflection magnitude and phase to the measured frequency spectra, as well as the influence of signal processing were investigated. We present a method to extract the phase of the reflection coefficients from the phase response of the frequency spectra and their integration into the presentation of the measurement data. The phase information significantly improved the detectability of the temporal evolution of the snow surface reflection. We developed an automated and a semi-automated snow surface tracking algorithm. Results were compared with independently measured snow height from a laser snow-depth sensor and results derived from an upward-looking impulse radar system (upGPR). The semi-automated tracking used the phase information and had an accuracy of about 6 to 8cm for dry-snow conditions, similar to the accuracy of the upGPR, compared to measurements from the laser snow-depth sensor. The percolation of water was observable in the radargrams. Results suggest that the upward-looking FMCW system may be a valuable alternative to conventional snow-depth sensors for locations, where fixed installations above ground are not feasible. •Snowpack measurement with upward-looking FMCW radar•Method to extract the phase of the reflection coefficients•Include phase into the illustration of the measurement data•Automated and semi-automated snow surface tracking algorithm•Improved snow surface tracking when using the phase of the reflection coefficients</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>FMCW</subject><subject>Geophysics. Techniques, methods, instrumentation and models</subject><subject>Lasers</subject><subject>Radar</subject><subject>Reflection</subject><subject>Sensors</subject><subject>Snow</subject><subject>Snow avalanches</subject><subject>Snow stratigraphy</subject><subject>Snow. Ice. Glaciers</subject><subject>Snowpack</subject><subject>Snowpack monitoring</subject><subject>Surface tracking</subject><subject>Tracking</subject><issn>0165-232X</issn><issn>1872-7441</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkU2LFDEQhoMo7rj6F6Q9CF66rXx0J_EgyOCqMOLFRW8hnY8xY08yJj2z-O_NMOO6nvRUFPXUSxUPQs8wdBjw8HLTmTTZ7NYhxdIRwKwD2gEM99ACC05azhi-jxaV7VtCydcL9KiUDdRe9vQhuiBMSiYZXaBX17sbnW07pfQ9xHWzakcdbXP1cfmlydrq3PiUmxLTTWPSweVmm2KYU67sY_TA66m4J-d6ia6v3n5evm9Xn959WL5Ztabncm6FAUcoltyMgLX24KgAzzUlnjhjqIf6AAY_yrE2lpKR4l5gKySh0uiRXqLXp9zdftw6a1ycs57ULoetzj9V0kH9PYnhm1qng2LA-l7IGvDiHJDTj70rs9qGYtw06ejSvigsABjHYuD_Rjkfhp5yckTlCTU5lZKdv70IgzpqUht1R5M6alJAVdVUd5_efel287eXCjw_A7oYPfmsownlDycY7wWwyi1PnKsCDsFlVUxw0TgbsjOzsin8xzm_ADa-tuw</recordid><startdate>20140701</startdate><enddate>20140701</enddate><creator>Okorn, Robert</creator><creator>Brunnhofer, Georg</creator><creator>Platzer, Thomas</creator><creator>Heilig, Achim</creator><creator>Schmid, Lino</creator><creator>Mitterer, Christoph</creator><creator>Schweizer, Jürg</creator><creator>Eisen, Olaf</creator><general>Elsevier B.V</general><general>Elsevier</general><general>Elsevier Scientific Pub. Co</general><scope>6I.</scope><scope>AAFTH</scope><scope>IQODW</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>5PM</scope><orcidid>https://orcid.org/0000-0001-5076-2968</orcidid><orcidid>https://orcid.org/0000-0001-9826-4191</orcidid></search><sort><creationdate>20140701</creationdate><title>Upward-looking L-band FMCW radar for snow cover monitoring</title><author>Okorn, Robert ; Brunnhofer, Georg ; Platzer, Thomas ; Heilig, Achim ; Schmid, Lino ; Mitterer, Christoph ; Schweizer, Jürg ; Eisen, Olaf</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c579t-8c0e23197cb01aaf0e380f7a32f2ecc3f020110fb9bc3fd32b31581d89239cab3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>FMCW</topic><topic>Geophysics. Techniques, methods, instrumentation and models</topic><topic>Lasers</topic><topic>Radar</topic><topic>Reflection</topic><topic>Sensors</topic><topic>Snow</topic><topic>Snow avalanches</topic><topic>Snow stratigraphy</topic><topic>Snow. Ice. Glaciers</topic><topic>Snowpack</topic><topic>Snowpack monitoring</topic><topic>Surface tracking</topic><topic>Tracking</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Okorn, Robert</creatorcontrib><creatorcontrib>Brunnhofer, Georg</creatorcontrib><creatorcontrib>Platzer, Thomas</creatorcontrib><creatorcontrib>Heilig, Achim</creatorcontrib><creatorcontrib>Schmid, Lino</creatorcontrib><creatorcontrib>Mitterer, Christoph</creatorcontrib><creatorcontrib>Schweizer, Jürg</creatorcontrib><creatorcontrib>Eisen, Olaf</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>Pascal-Francis</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Mechanical &amp; Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Cold regions science and technology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Okorn, Robert</au><au>Brunnhofer, Georg</au><au>Platzer, Thomas</au><au>Heilig, Achim</au><au>Schmid, Lino</au><au>Mitterer, Christoph</au><au>Schweizer, Jürg</au><au>Eisen, Olaf</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Upward-looking L-band FMCW radar for snow cover monitoring</atitle><jtitle>Cold regions science and technology</jtitle><addtitle>Cold Reg Sci Technol</addtitle><date>2014-07-01</date><risdate>2014</risdate><volume>103</volume><issue>100</issue><spage>31</spage><epage>40</epage><pages>31-40</pages><issn>0165-232X</issn><eissn>1872-7441</eissn><coden>CRSTDL</coden><abstract>Forecasting snow avalanche danger in mountainous regions is of major importance for the protection of infrastructure in avalanche run-out zones. Inexpensive measurement devices capable of measuring snow height and layer properties in avalanche starting zones may help to improve the quality of risk assessment. We present a low-cost L-band frequency modulated continuous wave radar system (FMCW) in upward-looking configuration. To monitor the snowpack evolution, the radar system was deployed in fall and subsequently was covered by snowfalls. During two winter seasons we recorded reflections from the overlying snowpack. The influence of reflection magnitude and phase to the measured frequency spectra, as well as the influence of signal processing were investigated. We present a method to extract the phase of the reflection coefficients from the phase response of the frequency spectra and their integration into the presentation of the measurement data. The phase information significantly improved the detectability of the temporal evolution of the snow surface reflection. We developed an automated and a semi-automated snow surface tracking algorithm. Results were compared with independently measured snow height from a laser snow-depth sensor and results derived from an upward-looking impulse radar system (upGPR). The semi-automated tracking used the phase information and had an accuracy of about 6 to 8cm for dry-snow conditions, similar to the accuracy of the upGPR, compared to measurements from the laser snow-depth sensor. The percolation of water was observable in the radargrams. Results suggest that the upward-looking FMCW system may be a valuable alternative to conventional snow-depth sensors for locations, where fixed installations above ground are not feasible. •Snowpack measurement with upward-looking FMCW radar•Method to extract the phase of the reflection coefficients•Include phase into the illustration of the measurement data•Automated and semi-automated snow surface tracking algorithm•Improved snow surface tracking when using the phase of the reflection coefficients</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><pmid>24994943</pmid><doi>10.1016/j.coldregions.2014.03.006</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0001-5076-2968</orcidid><orcidid>https://orcid.org/0000-0001-9826-4191</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0165-232X
ispartof Cold regions science and technology, 2014-07, Vol.103 (100), p.31-40
issn 0165-232X
1872-7441
language eng
recordid cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4045589
source Access via ScienceDirect (Elsevier)
subjects Earth, ocean, space
Exact sciences and technology
External geophysics
FMCW
Geophysics. Techniques, methods, instrumentation and models
Lasers
Radar
Reflection
Sensors
Snow
Snow avalanches
Snow stratigraphy
Snow. Ice. Glaciers
Snowpack
Snowpack monitoring
Surface tracking
Tracking
title Upward-looking L-band FMCW radar for snow cover monitoring
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-24T18%3A42%3A09IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_pubme&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Upward-looking%20L-band%20FMCW%20radar%20for%20snow%20cover%20monitoring&rft.jtitle=Cold%20regions%20science%20and%20technology&rft.au=Okorn,%20Robert&rft.date=2014-07-01&rft.volume=103&rft.issue=100&rft.spage=31&rft.epage=40&rft.pages=31-40&rft.issn=0165-232X&rft.eissn=1872-7441&rft.coden=CRSTDL&rft_id=info:doi/10.1016/j.coldregions.2014.03.006&rft_dat=%3Cproquest_pubme%3E1776653727%3C/proquest_pubme%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1776653727&rft_id=info:pmid/24994943&rft_els_id=S0165232X14000615&rfr_iscdi=true