Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide

Abstract The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measu...

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Main Authors: Xie Hu, Zhong Lu, Thomas C. Pierson, Rebecca Kramer, David L. George
Format: Article
Language:English
Published: Wiley 2018-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2017GL076623
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author Xie Hu
Zhong Lu
Thomas C. Pierson
Rebecca Kramer
David L. George
author_facet Xie Hu
Zhong Lu
Thomas C. Pierson
Rebecca Kramer
David L. George
author_sort Xie Hu
collection DOAJ
description Abstract The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measurements tied to only a few specific measurement sites. This approach is applied to an ~4 km2 reactivated translational landslide in the Columbia River Gorge (Washington State), which moves mainly during the winter rainy season. Results reveal the complex three‐dimensional shape of the landslide mass, how onset of sliding relates to cumulative rainfall, how surface velocity during sliding varies with location on the topographically complex landslide surface, and how the ground surface subsides slightly in weeks prior to downslope sliding.
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issn 0094-8276
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publishDate 2018-02-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-d19a56af07ed4e3097df8bf3488d6cd32025-08-20T02:31:40ZengWileyGeophysical Research Letters0094-82761944-80072018-02-014531453146210.1002/2017GL076623Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational LandslideXie Hu0Zhong Lu1Thomas C. Pierson2Rebecca Kramer3David L. George4Huffington Department of Earth Sciences Southern Methodist University Dallas TX USAHuffington Department of Earth Sciences Southern Methodist University Dallas TX USAU.S. Geological Survey Vancouver WA USAU.S. Geological Survey Vancouver WA USAU.S. Geological Survey Vancouver WA USAAbstract The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measurements tied to only a few specific measurement sites. This approach is applied to an ~4 km2 reactivated translational landslide in the Columbia River Gorge (Washington State), which moves mainly during the winter rainy season. Results reveal the complex three‐dimensional shape of the landslide mass, how onset of sliding relates to cumulative rainfall, how surface velocity during sliding varies with location on the topographically complex landslide surface, and how the ground surface subsides slightly in weeks prior to downslope sliding.https://doi.org/10.1002/2017GL076623Crescent Lake landslideInterferometric Synthetic Aperture Radar (InSAR)Global Positioning System (GPS)Transient landslide movement3D displacementLandslide thickness
spellingShingle Xie Hu
Zhong Lu
Thomas C. Pierson
Rebecca Kramer
David L. George
Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
Geophysical Research Letters
Crescent Lake landslide
Interferometric Synthetic Aperture Radar (InSAR)
Global Positioning System (GPS)
Transient landslide movement
3D displacement
Landslide thickness
title Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
title_full Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
title_fullStr Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
title_full_unstemmed Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
title_short Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide
title_sort combining insar and gps to determine transient movement and thickness of a seasonally active low gradient translational landslide
topic Crescent Lake landslide
Interferometric Synthetic Aperture Radar (InSAR)
Global Positioning System (GPS)
Transient landslide movement
3D displacement
Landslide thickness
url https://doi.org/10.1002/2017GL076623
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