Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations
During the Last Glacial Maximum (LGM), vast ice sheets covered part of the Northern Hemisphere. In Europe, the European Ice Sheet Complex (EISC) spanned form the British Islands to the Taymyr Peninsula in Siberia. There are considerable gaps in our knowledge of the EISC, specially in the extend and...
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fttudelft:oai:tudelft.nl:uuid:a8f4deee-a19c-4eac-906a-c28f7bb0b390 2023-07-30T04:04:11+02:00 Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations Rovira Navarro, Marc (author) van der Wal, W. (mentor) Barletta, Valentin Roberta (mentor) Sandberg Sørensen, Louise (mentor) Delft University of Technology (degree granting institution) 2017-09-01 http://resolver.tudelft.nl/uuid:a8f4deee-a19c-4eac-906a-c28f7bb0b390 en eng http://resolver.tudelft.nl/uuid:a8f4deee-a19c-4eac-906a-c28f7bb0b390 © 2017 Marc Rovira Navarro GRACE Glacial Isostatic Adjustment Barents and Kara Sea Solid Earth master thesis 2017 fttudelft 2023-07-08T20:17:26Z During the Last Glacial Maximum (LGM), vast ice sheets covered part of the Northern Hemisphere. In Europe, the European Ice Sheet Complex (EISC) spanned form the British Islands to the Taymyr Peninsula in Siberia. There are considerable gaps in our knowledge of the EISC, specially in the extend and deglaciation of the Svalbard-Barents-Kara Sea Ice Sheet (SBKIS). The fingerprint of the SBKIS is still visible through Glacial Isostatic Adjustment (GIA), the viscous rearranging of Earth's interior due to a changing surface load. The slow mass-flow from the borders of the paleo-ice sheet towards its center induces a secular change of the gravity field that can be observed using gravity data from the GRACE mission. We use GRACE data to obtain gravity disturbance rates and their uncertainty in the Barents and Kara Sea and compare these observations against modeled gravity rates for different combinations of ice deglaciation histories and Earth rheological parameters. Aerospace Engineering Master Thesis Ice Sheet Kara Sea Sea ice Svalbard Taymyr Taymyr Peninsula Siberia Delft University of Technology: Institutional Repository Kara Sea Svalbard Taymyr ENVELOPE(89.987,89.987,68.219,68.219) |
institution |
Open Polar |
collection |
Delft University of Technology: Institutional Repository |
op_collection_id |
fttudelft |
language |
English |
topic |
GRACE Glacial Isostatic Adjustment Barents and Kara Sea Solid Earth |
spellingShingle |
GRACE Glacial Isostatic Adjustment Barents and Kara Sea Solid Earth Rovira Navarro, Marc (author) Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
topic_facet |
GRACE Glacial Isostatic Adjustment Barents and Kara Sea Solid Earth |
description |
During the Last Glacial Maximum (LGM), vast ice sheets covered part of the Northern Hemisphere. In Europe, the European Ice Sheet Complex (EISC) spanned form the British Islands to the Taymyr Peninsula in Siberia. There are considerable gaps in our knowledge of the EISC, specially in the extend and deglaciation of the Svalbard-Barents-Kara Sea Ice Sheet (SBKIS). The fingerprint of the SBKIS is still visible through Glacial Isostatic Adjustment (GIA), the viscous rearranging of Earth's interior due to a changing surface load. The slow mass-flow from the borders of the paleo-ice sheet towards its center induces a secular change of the gravity field that can be observed using gravity data from the GRACE mission. We use GRACE data to obtain gravity disturbance rates and their uncertainty in the Barents and Kara Sea and compare these observations against modeled gravity rates for different combinations of ice deglaciation histories and Earth rheological parameters. Aerospace Engineering |
author2 |
van der Wal, W. (mentor) Barletta, Valentin Roberta (mentor) Sandberg Sørensen, Louise (mentor) Delft University of Technology (degree granting institution) |
format |
Master Thesis |
author |
Rovira Navarro, Marc (author) |
author_facet |
Rovira Navarro, Marc (author) |
author_sort |
Rovira Navarro, Marc (author) |
title |
Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
title_short |
Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
title_full |
Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
title_fullStr |
Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
title_full_unstemmed |
Studying the Svalbard-Barents-Kara Ice Sheet using GRACE observations |
title_sort |
studying the svalbard-barents-kara ice sheet using grace observations |
publishDate |
2017 |
url |
http://resolver.tudelft.nl/uuid:a8f4deee-a19c-4eac-906a-c28f7bb0b390 |
long_lat |
ENVELOPE(89.987,89.987,68.219,68.219) |
geographic |
Kara Sea Svalbard Taymyr |
geographic_facet |
Kara Sea Svalbard Taymyr |
genre |
Ice Sheet Kara Sea Sea ice Svalbard Taymyr Taymyr Peninsula Siberia |
genre_facet |
Ice Sheet Kara Sea Sea ice Svalbard Taymyr Taymyr Peninsula Siberia |
op_relation |
http://resolver.tudelft.nl/uuid:a8f4deee-a19c-4eac-906a-c28f7bb0b390 |
op_rights |
© 2017 Marc Rovira Navarro |
_version_ |
1772815411005358080 |