Inverse Level-set Problems for Capturing Calving Fronts

Capturing the calving front motion is critical for simulations of ice sheets and ice shelves. Multiple physical processes - besides calving also melting and the forward movement of the ice - need to be understood to accurately model the front. Calving is particularly challenging due to its discontin...

Full description

Bibliographic Details
Main Authors: Abele, Daniel, Basermann, Achim, Bungartz, Hans-Joachim, Humbert, Angelika
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://elib.dlr.de/199938/
https://elib.dlr.de/199938/1/AIP_Poster_A0.pdf
id ftdlr:oai:elib.dlr.de:199938
record_format openpolar
spelling ftdlr:oai:elib.dlr.de:199938 2024-05-19T07:31:39+00:00 Inverse Level-set Problems for Capturing Calving Fronts Abele, Daniel Basermann, Achim Bungartz, Hans-Joachim Humbert, Angelika 2023-09 application/pdf https://elib.dlr.de/199938/ https://elib.dlr.de/199938/1/AIP_Poster_A0.pdf en eng https://elib.dlr.de/199938/1/AIP_Poster_A0.pdf Abele, Daniel und Basermann, Achim und Bungartz, Hans-Joachim und Humbert, Angelika (2023) Inverse Level-set Problems for Capturing Calving Fronts. In: 11th Applied Inverse Problems Conference. 11th Applied Inverse Problems Conference, 2023-09-04 - 2023-09-08, Göttingen, Germany. High-Performance Computing Institut für Softwaretechnologie Konferenzbeitrag NonPeerReviewed 2023 ftdlr 2024-04-25T01:11:02Z Capturing the calving front motion is critical for simulations of ice sheets and ice shelves. Multiple physical processes - besides calving also melting and the forward movement of the ice - need to be understood to accurately model the front. Calving is particularly challenging due to its discontinuous nature and modelers require more tools to examine it. A common technique for capturing the front in ice simulations is the Level-set method. The front is represented implicitly by the zero isoline of a function. The movement of the front is described by an advection equation, where the velocity field is a combination of ice velocity and frontal ablation rate. To improve understanding of these processes, we are developing methods to estimate parameters of calving laws based on inverse Level-Set problems. The regularization is chosen so it can handle discontinuous parameters or calving laws to fit discontinuous front positions due to large calving events. The input for the inverse problem is formed by observational data from satellite images that is often sparse. The methods will be applied to large scale models of the Antarctic Ice Sheet. Conference Object Antarc* Antarctic Ice Sheet Ice Shelves German Aerospace Center: elib - DLR electronic library
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language English
topic High-Performance Computing
Institut für Softwaretechnologie
spellingShingle High-Performance Computing
Institut für Softwaretechnologie
Abele, Daniel
Basermann, Achim
Bungartz, Hans-Joachim
Humbert, Angelika
Inverse Level-set Problems for Capturing Calving Fronts
topic_facet High-Performance Computing
Institut für Softwaretechnologie
description Capturing the calving front motion is critical for simulations of ice sheets and ice shelves. Multiple physical processes - besides calving also melting and the forward movement of the ice - need to be understood to accurately model the front. Calving is particularly challenging due to its discontinuous nature and modelers require more tools to examine it. A common technique for capturing the front in ice simulations is the Level-set method. The front is represented implicitly by the zero isoline of a function. The movement of the front is described by an advection equation, where the velocity field is a combination of ice velocity and frontal ablation rate. To improve understanding of these processes, we are developing methods to estimate parameters of calving laws based on inverse Level-Set problems. The regularization is chosen so it can handle discontinuous parameters or calving laws to fit discontinuous front positions due to large calving events. The input for the inverse problem is formed by observational data from satellite images that is often sparse. The methods will be applied to large scale models of the Antarctic Ice Sheet.
format Conference Object
author Abele, Daniel
Basermann, Achim
Bungartz, Hans-Joachim
Humbert, Angelika
author_facet Abele, Daniel
Basermann, Achim
Bungartz, Hans-Joachim
Humbert, Angelika
author_sort Abele, Daniel
title Inverse Level-set Problems for Capturing Calving Fronts
title_short Inverse Level-set Problems for Capturing Calving Fronts
title_full Inverse Level-set Problems for Capturing Calving Fronts
title_fullStr Inverse Level-set Problems for Capturing Calving Fronts
title_full_unstemmed Inverse Level-set Problems for Capturing Calving Fronts
title_sort inverse level-set problems for capturing calving fronts
publishDate 2023
url https://elib.dlr.de/199938/
https://elib.dlr.de/199938/1/AIP_Poster_A0.pdf
genre Antarc*
Antarctic
Ice Sheet
Ice Shelves
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelves
op_relation https://elib.dlr.de/199938/1/AIP_Poster_A0.pdf
Abele, Daniel und Basermann, Achim und Bungartz, Hans-Joachim und Humbert, Angelika (2023) Inverse Level-set Problems for Capturing Calving Fronts. In: 11th Applied Inverse Problems Conference. 11th Applied Inverse Problems Conference, 2023-09-04 - 2023-09-08, Göttingen, Germany.
_version_ 1799469523984711680