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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Xie Hu</dc:contributor>
  <dc:contributor>Nicholas Sitar</dc:contributor>
  <dc:contributor>Robert Kayen</dc:contributor>
  <dc:contributor>Shengwen Qi</dc:contributor>
  <dc:contributor>Houjun Jiang</dc:contributor>
  <dc:contributor>Xudong Wang</dc:contributor>
  <dc:creator>Xuguo Shi</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts u-font-serif"&gt;&lt;div id="ab0005" class="abstract author" lang="en"&gt;&lt;div id="as0005"&gt;&lt;p id="sp0050"&gt;&lt;span&gt;Landslides are common geohazards associated with natural drivers such as precipitation,&amp;nbsp;land degradation, toe erosion by rivers and wave attack, and ground shaking. On the other hand, human alterations such as inundation by water&amp;nbsp;impoundment&amp;nbsp;or rapid drawdown may also destabilize the surrounding slopes. The Guobu slope is an ancient rockslide on the banks of the Laxiwa&amp;nbsp;hydropower station&amp;nbsp;reservoir (China), which reactivated during the&amp;nbsp;reservoir impoundment&amp;nbsp;in 2009. We extracted three-dimensional surface displacements with azimuth and range&amp;nbsp;radar interferometry&amp;nbsp;using European Space Agency's Copernicus Sentinel-1 and German Aerospace Center's TerraSAR-X data during 20152019. The upper part of the Guobu rockslide is characterized by toppling and is mostly subsiding with maximum rates over 0.4&amp;nbsp;m/yr and 0.7&amp;nbsp;m/yr in the vertical and horizontal directions, respectively. During filling of the reservoir prior to 2014, there was a long-wavelength in-phase response between rising reservoir level and GPS-observed increased slope movements. After the reservoir water level stabilized from 2015 to 2019, the slide movement became seasonal and we see a correlation between rainfall and landslide movement. These observations suggest that the slide motion is now primarily controlled by rainfall. The spatiotemporal landslide displacements allow us to estimate the hydraulic&amp;nbsp;diffusivity&amp;nbsp;of the rock mass, to be on the order (~1.05&amp;nbsp;×&amp;nbsp;10&lt;/span&gt;&lt;sup&gt;‐7&lt;/sup&gt;&amp;nbsp;m&lt;sup&gt;2&lt;/sup&gt;/s) and the thickness of the moving rock mass (~200&amp;nbsp;m). Our results demonstrate that InSAR is a useful tool for monitoring the rockslide movement as a function of seasonal precipitation.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.rse.2021.112664</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Hydrological control shift from river level to rainfall in the reactivated Guobu slope besides the Laxiwa hydropower station in China</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>