date: 2022-08-23T08:52:59Z pdf:PDFVersion: 1.7 pdf:docinfo:title: Inferring Mass Loss by Measuring Contemporaneous Deformation around the Helheim Glacier, Southeastern Greenland, Using Sentinel-1 InSAR xmp:CreatorTool: LaTeX with hyperref Keywords: Helheim glacier; isostatic rebound; mass loss; Sentinel-1A; InSAR access_permission:modify_annotations: true access_permission:can_print_degraded: true subject: The elastic response of solid earth to glacier and ice sheet melting, the most important consequences of climate change, is a contemporaneous uplift. Here, we use interferometric synthetic aperture radar (InSAR) measurements to detect crustal deformation and mass loss near the Helheim glacier, one of the largest glaciers in southeastern Greenland. The InSAR time series of Sentinel-1 data between April 2016 and July 2020 suggest that there is a maximum cumulative displacement of ~6 cm in the line of sight (LOS) direction from the satellite to the ground near Helheim. We use an exponentially decreasing model of the thinning rate, which assumes that the mass loss starts at the lower-elevation terminal region of the glacier and continues to the higher-elevation interior. A linear inversion of the derived crustal uplift in the vicinity of bedrock using this model for surface loading in an elastic half-space suggests a mass loss of 8.33 Gt/year, which agrees with the results from other studies. dc:creator: Zohreh Erfani Jazi, Mahdi Motagh and Volker Klemann dcterms:created: 2022-08-23T06:58:11Z Last-Modified: 2022-08-23T08:52:59Z dcterms:modified: 2022-08-23T08:52:59Z dc:format: application/pdf; version=1.7 title: Inferring Mass Loss by Measuring Contemporaneous Deformation around the Helheim Glacier, Southeastern Greenland, Using Sentinel-1 InSAR Last-Save-Date: 2022-08-23T08:52:59Z pdf:docinfo:creator_tool: LaTeX with hyperref access_permission:fill_in_form: true pdf:docinfo:keywords: Helheim glacier; isostatic rebound; mass loss; Sentinel-1A; InSAR pdf:docinfo:modified: 2022-08-23T08:52:59Z meta:save-date: 2022-08-23T08:52:59Z pdf:encrypted: false dc:title: Inferring Mass Loss by Measuring Contemporaneous Deformation around the Helheim Glacier, Southeastern Greenland, Using Sentinel-1 InSAR modified: 2022-08-23T08:52:59Z cp:subject: The elastic response of solid earth to glacier and ice sheet melting, the most important consequences of climate change, is a contemporaneous uplift. Here, we use interferometric synthetic aperture radar (InSAR) measurements to detect crustal deformation and mass loss near the Helheim glacier, one of the largest glaciers in southeastern Greenland. The InSAR time series of Sentinel-1 data between April 2016 and July 2020 suggest that there is a maximum cumulative displacement of ~6 cm in the line of sight (LOS) direction from the satellite to the ground near Helheim. We use an exponentially decreasing model of the thinning rate, which assumes that the mass loss starts at the lower-elevation terminal region of the glacier and continues to the higher-elevation interior. A linear inversion of the derived crustal uplift in the vicinity of bedrock using this model for surface loading in an elastic half-space suggests a mass loss of 8.33 Gt/year, which agrees with the results from other studies. pdf:docinfo:subject: The elastic response of solid earth to glacier and ice sheet melting, the most important consequences of climate change, is a contemporaneous uplift. Here, we use interferometric synthetic aperture radar (InSAR) measurements to detect crustal deformation and mass loss near the Helheim glacier, one of the largest glaciers in southeastern Greenland. The InSAR time series of Sentinel-1 data between April 2016 and July 2020 suggest that there is a maximum cumulative displacement of ~6 cm in the line of sight (LOS) direction from the satellite to the ground near Helheim. We use an exponentially decreasing model of the thinning rate, which assumes that the mass loss starts at the lower-elevation terminal region of the glacier and continues to the higher-elevation interior. A linear inversion of the derived crustal uplift in the vicinity of bedrock using this model for surface loading in an elastic half-space suggests a mass loss of 8.33 Gt/year, which agrees with the results from other studies. Content-Type: application/pdf pdf:docinfo:creator: Zohreh Erfani Jazi, Mahdi Motagh and Volker Klemann X-Parsed-By: org.apache.tika.parser.DefaultParser creator: Zohreh Erfani Jazi, Mahdi Motagh and Volker Klemann meta:author: Zohreh Erfani Jazi, Mahdi Motagh and Volker Klemann dc:subject: Helheim glacier; isostatic rebound; mass loss; Sentinel-1A; InSAR meta:creation-date: 2022-08-23T06:58:11Z created: Tue Aug 23 08:58:11 CEST 2022 access_permission:extract_for_accessibility: true access_permission:assemble_document: true xmpTPg:NPages: 20 Creation-Date: 2022-08-23T06:58:11Z access_permission:extract_content: true access_permission:can_print: true meta:keyword: Helheim glacier; isostatic rebound; mass loss; Sentinel-1A; InSAR Author: Zohreh Erfani Jazi, Mahdi Motagh and Volker Klemann producer: pdfTeX-1.40.21 access_permission:can_modify: true pdf:docinfo:producer: pdfTeX-1.40.21 pdf:docinfo:created: 2022-08-23T06:58:11Z