High-Resolution DEM Generation from Spaceborne and Terrestrial Remote Sensing Data for Improved Volcano Hazard Assessment — A Case Study at Nevado del Ruiz, Colombia

Fanghui Deng, Mel Rodgers, Surui Xie, Timothy Dixon, Sylvain J. Charbonnier, Elisabeth Gallant, Christian Mauricio López Vélez, Milton Ordoñez, Rocco Malservisi, Nicholas K. Voss, Jacob A. Richardson

Research output: Contribution to journalArticlepeer-review

Abstract

<p> <p id="x-x-sp0115"> Volcanoes with rugged terrain remain a challenging target for generating high-resolution digital elevation models (DEMs), especially in tropical areas with frequent cloud cover. Using Nevado del Ruiz volcano as an example, we combined DEMs from the TanDEM-X (TDX) satellite mission, terrestrial radar interferometry (TRI), and Structure from Motion (SfM), to generate a new DEM with 10-m spatial resolution. This is the first study combining satellite radar, ground-based radar, photography, and freely available global DEMs to generate a high-resolution DEM without data gaps. TDX data from ascending and descending orbits were combined to generate the base DEM. Instead of using a raster format to fuse DEMs generated from different data sets with different resolutions, we developed a methodology based on 3-D point clouds: 1) re-georeference the 5-m TRI and ~1-m SfM DEMs to the 10-m TDX DEM using the iterative closest point (ICP) algorithm to minimize the horizontal and vertical discrepancy between DEMs; then 2) merge the multiple point clouds to generate a final DEM without data gaps using an adaptive algorithm that uses two search distances to smooth the transition at the edges of different data sets. We assess the new 10-m DEM by comparing simulated inundation zones obtained with two volcano flow models, LaharZ (for lahars) and VolcFlow (for pyroclastic flows), and find significant differences with respect to the 30-m SRTM DEM. Our LaharZ simulation over the new DEM shows a longer lahar run-out distance. For pyroclastic flows, the VolcFlow simulation over the new DEM produces highly channelized flows over the steep portions of a river channel and gives a larger extent of thicker deposits compared to those obtained with the 30-m SRTM DEM. Quantitative and qualitative geomorphic analysis suggests that up-to-date DEMs with high spatial resolution (~ 10 m or even better) need to be generated to improve volcano hazard assessment for active volcanoes. </p></p>
Original languageAmerican English
JournalRemote Sensing of Environment
Volume233
DOIs
StatePublished - Nov 1 2019

Keywords

  • Nevado del Ruiz
  • Digital elevation model
  • TanDEM-XInSAR
  • Terrestrial radar interferometry
  • Structure from motion
  • DEM fusion
  • Volcanic flow modeling

Disciplines

  • Earth Sciences

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