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Practical Application of Satellite-Based SAR Interferometry for the Detection of Landslide Activity

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F15%3A86094069" target="_blank" >RIV/61989100:27350/15:86094069 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/68407700:21110/15:00242178 RIV/61989100:27740/15:86094069

  • Výsledek na webu

    <a href="http://www.sciencedirect.com/science/article/pii/S1878522015003768" target="_blank" >http://www.sciencedirect.com/science/article/pii/S1878522015003768</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.proeps.2015.08.113" target="_blank" >10.1016/j.proeps.2015.08.113</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Practical Application of Satellite-Based SAR Interferometry for the Detection of Landslide Activity

  • Popis výsledku v původním jazyce

    After two decades of SAR satellite operation, their data, processed by interferometric techniques (InSAR), allows for a sensitive detection of terrain movements. Various projects have risen towards the detection of landslide activity and thus possibility of early warning system based on SAR data. The ability of InSAR techniques to detect a slope stability is limited and depends on slope orientation, movement rate, vegetation cover and temporal and spatial image resolution. This paper presents common issues found in past projects of the team of authors observing landslides using available satellite SAR data processed by various InSAR techniques. It is demonstrated that in some cases the basic differential InSAR combining only two images provides more valuable information compared to advance multi-temporal InSAR techniques. The paper aims at providing guidelines for maximal successful detection of landslide activity and to introduce pros and cons of the InSAR method, which often discussed in geology and geophysics circles. We prove the potential of techniques using satellite-based InSAR to identify creeping movement of structures built at moving slopes and the limited possibility to detect movements at moderately vegetated slopes by using especially the L-band or a combination of winter-season SAR and other images within very short temporal difference. It is possible to overcome misinterpretation of results by proper understanding of InSAR source phase component at slopes, including phase distortions due to SAR geometry, vegetation movement (vegetated mass movement) and atmospheric pressure changes correlated with height differences.

  • Název v anglickém jazyce

    Practical Application of Satellite-Based SAR Interferometry for the Detection of Landslide Activity

  • Popis výsledku anglicky

    After two decades of SAR satellite operation, their data, processed by interferometric techniques (InSAR), allows for a sensitive detection of terrain movements. Various projects have risen towards the detection of landslide activity and thus possibility of early warning system based on SAR data. The ability of InSAR techniques to detect a slope stability is limited and depends on slope orientation, movement rate, vegetation cover and temporal and spatial image resolution. This paper presents common issues found in past projects of the team of authors observing landslides using available satellite SAR data processed by various InSAR techniques. It is demonstrated that in some cases the basic differential InSAR combining only two images provides more valuable information compared to advance multi-temporal InSAR techniques. The paper aims at providing guidelines for maximal successful detection of landslide activity and to introduce pros and cons of the InSAR method, which often discussed in geology and geophysics circles. We prove the potential of techniques using satellite-based InSAR to identify creeping movement of structures built at moving slopes and the limited possibility to detect movements at moderately vegetated slopes by using especially the L-band or a combination of winter-season SAR and other images within very short temporal difference. It is possible to overcome misinterpretation of results by proper understanding of InSAR source phase component at slopes, including phase distortions due to SAR geometry, vegetation movement (vegetated mass movement) and atmospheric pressure changes correlated with height differences.

Klasifikace

  • Druh

    D - Stať ve sborníku

  • CEP obor

    IN - Informatika

  • OECD FORD obor

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Ostatní

  • Rok uplatnění

    2015

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název statě ve sborníku

    WMESS 2015 : World Multidisciplinary Earth Sciences Symposium : 07-11 September 2015, Czech Republic, Prague

  • ISBN

  • ISSN

    1878-5220

  • e-ISSN

  • Počet stran výsledku

    6

  • Strana od-do

    613-618

  • Název nakladatele

    [s.n.]

  • Místo vydání

    [Česko]

  • Místo konání akce

    Praha

  • Datum konání akce

    7. 9. 2015

  • Typ akce podle státní příslušnosti

    WRD - Celosvětová akce

  • Kód UT WoS článku

    000370751200095