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9 results for “Ground deformation”
Coseismic ground deformation map for the Mw5.7 20 March, 2019 Acipayam earthquake (Turkey)
<p>This repository contains an interferogram from Sentinel-1 satellite acquired over the Mw5.7 20 March, 2019 Acipayam earthquake (Turkey). This interferogram was obtained by processing Sentinel-1 SAR data with the JPL-developed InSAR Scientific Computing Environment (ISCE) open-source software package.</p> <p>Sentinel-1 descending track 138:</p> <ul> <li>Master image: 11 Mar 2019, identifier: S1A_IW_SLC_1SDV_20190311T040709_20190311T040736_026285_02F00C_6A73</li> <li>Slave image: 23 Mar 2019, identifier: S1A_IW_SLC_1SDV_20190323T040709_20190323T040736_026460_02F67D_EC68</li> </ul> <p>This interferogram was generated for figures in: Jiang, Y., and González, P. J. (2020). "Bayesian inversion of wrapped satellite interferometric phase to estimate fault and volcano surface ground deformation models. " JGR: Solid Earth.</p>
Coseismic ground deformation map for the 2020 M>7.5 Shumagin, Alaska, earthquake doublet
<p>This repository contains six interferograms from ESA Sentinel-1 satellite acquired over the 2020 M>7.5 Shumagin, Alaska, earthquake doublet. These interferograms were obtained by processing Sentinel-1 SAR data with the JPL-developed InSAR Scientific Computing Environment (ISCE) open-source software package. The details of six Sentinel-1 interferograms for the 2020 Shumagin earthquake doublet, M7.8 and M7.6 events, are listed in the table below.</p> <table> <tbody> <tr> <td> <p>Earthquake date and magnitude</p> </td> <td> <p>Track</p> <p>no.</p> </td> <td> <p>Direction</p> <p>(asc/des)</p> </td> <td> <p>Incidence</p> <p>(degree)</p> </td> <td> <p>Primary image</p> <p>(yyyy/mm/dd hh:mm:ss)</p> </td> <td> <p>Secondary image</p> <p>(yyyy/mm/dd hh:mm:ss)</p> </td> </tr> <tr> <td>2020/07/22 06:12:44 M7.8</td> <td>73</td> <td>des</td> <td>30-33</td> <td>2020/07/10 17:03:59</td> <td>2020/07/22 17:04:00</td> </tr> <tr> <td> </td> <td>102</td> <td>des</td> <td>43-46</td> <td>2020/07/12 16:47:32</td> <td>2020/07/24 16:47:33</td> </tr> <tr> <td> </td> <td>153</td> <td>asc</td> <td>36-41</td> <td>2020/07/22 04:23:36</td> <td>2020/09/08 04:23:39</td> </tr> <tr> <td>2020/10/19 20:54:38 M7.6</td> <td>73</td> <td>des</td> <td>30-35</td> <td>2020/10/14 17:04:04</td> <td>2020/10/26 17:04:04</td> </tr> <tr> <td> </td> <td>102</td> <td>des</td> <td>43-46</td> <td>2020/10/16 16:47:36</td> <td>2020/10/28 16:47:36</td> </tr> <tr> <td> </td> <td>153</td> <td>asc</td> <td>34-41</td> <td>2020/10/14 04:23:40</td> <td>2020/11/07 04:23:40</td> </tr> </tbody> </table> <p> </p> <p>These interferograms were generated for figures in: Jiang, Y., González, P. J., and Bürgmann, R. "Subduction earthquakes controlled by incoming plate geometry: The 2020 M>7.5 Shumagin, Alaska, earthquake doublet. " Earth and Planetary Science Letters.</p>
Pre-eruption ground deformation maps at Kilauea (Hawai`i, USA): 2014-2017 and 2018.
<p>Vertical displacement (velocity) maps of Kilauea (Hawai`i, USA) derived from InSAR, for the time periods 2014-2017 and 2018. Vertical velocity data were obtained by processing Sentinel-1 ascending and descending SAR data (tracks 124 and 87, respectively). Data were processed using the JPL-developed InSAR Scientific Computing Environment (ISCE) open-source software package, and further time-series analysis was performed using the MintPy software toolbox (Miami INsar Time-series software in PYthon), developed at the University of Miami. An SRTM-derived Digital Elevation Model is also provided. </p> <p>These data were generated for figures in: Farquharson, J. I. and Amelung, F. [2020], "<em>Extreme rainfall triggered the 2018 rift eruption at Kīlauea Volcano.</em>" <a href="https://doi.org/10.1038/s41586-020-2172-5">https://doi.org/10.1038/s41586-020-2172-5</a></p> <p> </p>
Dataset and figures for "Nationwide urban ground deformation monitoring in Japan using Sentinel-1 LiCSAR products and LiCSBAS"
<p>This dataset contains the deformation data for 191 data sets and figures (LOS velocities, amplitude and time offset of the annual deformation, decomposed vertical and EW velocities, rice paddy fields, NDVI, optical images, topography, and SB network) mentioned in the paper “Nationwide urban ground deformation monitoring in Japan using Sentinel-1 LiCSAR products and LiCSBAS”</p> <p>Morishita, Y. Nationwide urban ground deformation monitoring in Japan using Sentinel-1 LiCSAR products and LiCSBAS. <em>Prog Earth Planet Sci</em> <strong>8, </strong>6 (2021). https://doi.org/10.1186/s40645-020-00402-7</p> <p>View on a web map:</p> <p>https://yumorishita.github.io/gsimaps_S1_Japan_LiCSBAS/#9/35.766572/140.038605/&base=std&base_grayscale=1&ls=std%2C0.5%7Chillshademap%2C0.5%7CallUD%7Clanduse_veg&blend=100&disp=1110&vs=c1j0h0k0l0u0t0z0r0s0m0f2&d=m</p>
Ground deformation maps of the Visso and Norcia 2016 earthquakes captured from Sentinel-1 SAR
<p>The dataset contains the Line Of Sight (LOS) deformation maps obtained by applying Differential SAR Interferometry (DinSAR) to Sentinel-1 Interferometric Wide-swath (or TOPSAR) imagery.</p> <p>Two maps are provided: the first maps is the LOS deformation estimated from ascending data, the second map is the LOS deformation from descending images.</p> <p>Maps are expressed in metres and are provided in raster geotiff format.</p> <p>Data have been processed with GAMMA Interferometric processor.</p> <p>Ascending data details:</p> <p>SAR pairs are dated 2016/10/27 and 2016/11/02, acquired on relative orbit number 44, by Sentinel-1B and Sentinel-1A, respectively.</p> <p>The DEM used for removing the topographic phase is the SRTM 1 arc second. The interferogram has been generated by applying a 1x5 multi-look factor in azimuth and range, respectively.</p> <p>Final product has been geocoded in UTM WGS84 33 Nord projection, with a posting of 20 m.</p> <p>Descending data details:</p> <p>SAR pairs are dated 2016/10/26 and 2016/11/01, acquired on relative orbit number 22, by Sentinel-1B and Sentinel-1A, respectively.</p> <p>The DEM used for removing the topographic phase is the SRTM 1 arc second. The interferogram has been generated by applying a 2x10 multi-look factor in azimuth and range, respectively.</p> <p>Final product has been geocoded in UTM WGS84 33 Nord projection, with a posting of 40 m.</p>
Ground deformation maps of the Visso and Norcia (Italy) 2016 earthquakes from ALOS-2 SAR data
<p>The datasets consist of the Line of Sight (LoS) deformation maps obtained by applying Differential SAR Interferometry (DinSAR) to ALOS-2 (Strip Map acquisition mode) pairs.</p> <p>ALOS-2 is operated by the Japan Aerospace Exploration Agency (JAXA).</p> <p>Two maps were retrieved by processing data from both the ascending and descending track.</p> <p>Both the maps are in meters and provided in raster geotiff format.</p> <p>Data have been processed using the Sarscape© software.</p> <p>Ascending pair details:</p> <p>SAR images were acquired on 2016/08/24 and 2016/11/02, path 197, frame 850.</p> <p>The adopted DEM used for the topographic phase removal was the SRTM 1 arc second. The interferogram was generated by applying a 11x5 multi-look factor in azimuth and range, respectively.</p> <p>Final product were geocoded in UTM WGS84 33 Nord projection, and a final pixel size of 40 m.</p> <p>Descending pair details:</p> <p>SAR images were acquired on 2016/08/31 and 2016/11/09, path 92, frame 2750.</p> <p>The adopted DEM used for the topographic phase removal was the SRTM 1 arc second. The interferogram was generated by applying a 11x5 multi-look factor in azimuth and range, respectively.</p> <p>Final product were geocoded in UTM WGS84 33 Nord projection, and a final pixel size of 40 m.</p>
GNSS and levelling data to detect ground deformation along the Upper Adriatic Sea coastal area (Italy)
<p>This geodetic dataset includes both Global Navigation Satellite System (GNSS) and levelling data. GNSS measurements were recorded by continuous stations managed by public institutions and private companies, while levelling measurements were obtained by the use of benchmarks managed by ENI S.p.A. </p> <p>This dataset is used in the manuscript entitled "Multi-technique geodetic detection of onshore and offshore subsidence along the Upper Adriatic Sea coasts" to estimate deformation around the littoral area of Ravenna (Italy) (Polcari et al., 2022). The GNSS data, from permanent stations RAVE, PCTA, FIUN and ANGA covers the period from around 1998 to 2018. The files in .csv format contain displacement time series with respect to the Adria-fixed reference frame and for PCTA, FIUN and ANGA also with respect to RAVE GNSS station.</p> <p>The levelling data refer to campaigns that took place in 2002, 2003, 2004, 2005, 2007, 2009, 2011, 2014, and 2017. The file named <em>Original.csv</em> contains the original height measurements for each benchmark, while the file named <em>Ref.RAVE.csv</em> contains the mean velocity and the displacement calculated for all 147 benchmarks. In this last file the data were scaled with respect to the mean velocity of the benchmark located near the RAVE station.</p>
Ground deformation map for the 2011 Hawthorne seismic swarm (Nevada, USA)
<p>This repository contains eight interferograms from RADARSAT-2 and ENVISAT satellites acquired over the March-September, 2011 Hawthorne seismic swarm, Nevada (USA).</p> <p>Five interferograms were obtained by processing the Canadian Space Agency RADARSAT-2 SAR data along one ascending track (incidence angle 35<sup>◦</sup> and heading angle 350<sup>◦</sup>) with GAMMA software.</p> <ul> <li>20110322_HH_20110415_HH.adf.unw.grd</li> <li>20110226_HH_20110415_HH.adf.unw.grd</li> <li>20110322_HH_20110720_HH.adf.unw.grd</li> <li>20110415_HH_20110626_HH.adf.unw.grd</li> <li>20110315_HH_20110526_HH.adf.unw.grd</li> </ul> <p>Three interferograms were obtained by processing the European Space Agency ENVISAT SAR data along one descending track (incidence angle 35<sup>◦</sup> and heading angle -166<sup>◦</sup>) with DORIS software and ISCE software.</p> <ul> <li>20110320_20110618.lld.grd</li> <li>20110419_20110618.lld.grd</li> <li>20110718_20110916_filt_topophase.unw.geo</li> </ul> <p>These interferogram were generated for figures in: Jiang, Y., Samsonov, S. V., and González, P. J. (2021). "Aseismic fault slip nucleation during a shallow normal-faulting seismic swarm constrained using a physically-informed geodetic inversion method. " JGR: Solid Earth.</p>
Dataset and figures for "Nationwide urban ground deformation in Japan for 15 years detected by ALOS, Sentinel-1, and LiCSBAS"
<p>This dataset contains the LiCSBAS results and figures (LOS velocities, decomposed vertical and EW velocities, optical images, SB network, mask) mentioned in the paper “Nationwide urban ground deformation in Japan for 15 years detected by ALOS, Sentinel-1, and LiCSBAS”.</p>
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