Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ...
The northern Antarctic Peninsula is one of the fastest changing regions on Earth. The disintegration of the Larsen-A Ice Shelf in 1995 caused tributary glaciers to adjust by speeding up, surface lowering, and overall increased ice-mass discharge. In this study, we investigate the temporal variation...
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ftdatacite:10.1594/pangaea.859573 2024-09-15T17:47:22+00:00 Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... Seehaus, Thorsten Marinsek, Sebastián Helm, Veit Skvarca, Pedro Braun, Matthias Holger 2015 application/zip https://dx.doi.org/10.1594/pangaea.859573 https://doi.pangaea.de/10.1594/PANGAEA.859573 en eng PANGAEA https://store.pangaea.de/Publications/Seehaus-etal_2015/Data_Description_Seehaus_et_al_2015.pdf https://dx.doi.org/10.1016/j.epsl.2015.06.047 https://store.pangaea.de/Publications/Seehaus-etal_2015/Data_Description_Seehaus_et_al_2015.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Multiple investigations Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 dataset Supplementary Dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.85957310.1016/j.epsl.2015.06.047 2024-08-01T10:29:01Z The northern Antarctic Peninsula is one of the fastest changing regions on Earth. The disintegration of the Larsen-A Ice Shelf in 1995 caused tributary glaciers to adjust by speeding up, surface lowering, and overall increased ice-mass discharge. In this study, we investigate the temporal variation of these changes at the Dinsmoor-Bombardier-Edgeworth glacier system by analyzing dense time series from various spaceborne and airborne Earth observation missions. Precollapse ice shelf conditions and subsequent adjustments through 2014 were covered. Our results show a response of the glacier system some months after the breakup, reaching maximum surface velocities at the glacier front of up to 8.8 m/d in 1999 and a subsequent decrease to ~1.5 m/d in 2014. Using a dense time series of interferometrically derived TanDEM-X digital elevation models and photogrammetric data, an exponential function was fitted for the decrease in surface elevation. Elevation changes in areas below 1000 m a.s.l. amounted to at least ... : Supplement to: Seehaus, Thorsten; Marinsek, Sebastián; Helm, Veit; Skvarca, Pedro; Braun, Matthias Holger (2015): Changes in ice dynamics, elevation and mass discharge of Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula. Earth and Planetary Science Letters, 427, 125-135 ... Dataset Antarc* Antarctic Antarctic Peninsula Ice Shelf Sea ice DataCite |
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Open Polar |
collection |
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ftdatacite |
language |
English |
topic |
Multiple investigations Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Multiple investigations Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Seehaus, Thorsten Marinsek, Sebastián Helm, Veit Skvarca, Pedro Braun, Matthias Holger Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
topic_facet |
Multiple investigations Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The northern Antarctic Peninsula is one of the fastest changing regions on Earth. The disintegration of the Larsen-A Ice Shelf in 1995 caused tributary glaciers to adjust by speeding up, surface lowering, and overall increased ice-mass discharge. In this study, we investigate the temporal variation of these changes at the Dinsmoor-Bombardier-Edgeworth glacier system by analyzing dense time series from various spaceborne and airborne Earth observation missions. Precollapse ice shelf conditions and subsequent adjustments through 2014 were covered. Our results show a response of the glacier system some months after the breakup, reaching maximum surface velocities at the glacier front of up to 8.8 m/d in 1999 and a subsequent decrease to ~1.5 m/d in 2014. Using a dense time series of interferometrically derived TanDEM-X digital elevation models and photogrammetric data, an exponential function was fitted for the decrease in surface elevation. Elevation changes in areas below 1000 m a.s.l. amounted to at least ... : Supplement to: Seehaus, Thorsten; Marinsek, Sebastián; Helm, Veit; Skvarca, Pedro; Braun, Matthias Holger (2015): Changes in ice dynamics, elevation and mass discharge of Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula. Earth and Planetary Science Letters, 427, 125-135 ... |
format |
Dataset |
author |
Seehaus, Thorsten Marinsek, Sebastián Helm, Veit Skvarca, Pedro Braun, Matthias Holger |
author_facet |
Seehaus, Thorsten Marinsek, Sebastián Helm, Veit Skvarca, Pedro Braun, Matthias Holger |
author_sort |
Seehaus, Thorsten |
title |
Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
title_short |
Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
title_full |
Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
title_fullStr |
Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
title_full_unstemmed |
Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014) ... |
title_sort |
surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at dinsmoor-bombardier-edgeworth glacier system, antarctic peninsula (1992-2014) ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.859573 https://doi.pangaea.de/10.1594/PANGAEA.859573 |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Sea ice |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Sea ice |
op_relation |
https://store.pangaea.de/Publications/Seehaus-etal_2015/Data_Description_Seehaus_et_al_2015.pdf https://dx.doi.org/10.1016/j.epsl.2015.06.047 https://store.pangaea.de/Publications/Seehaus-etal_2015/Data_Description_Seehaus_et_al_2015.pdf |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.85957310.1016/j.epsl.2015.06.047 |
_version_ |
1810496574331027456 |