DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS

Abstract: In cooperation between remote sensing experts and cartographers interested in glaciology new types of maps showing the glacier dynamics have been developed. The map make use of the original phase gradient approach to glacier rheology modelling based on repeat-pass ERTS SAR interferograms....

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Main Authors: Manfred F. Buchroithner, Sebastian Walther
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.8834
http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.532.8834 2023-05-15T16:21:54+02:00 DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS Manfred F. Buchroithner Sebastian Walther The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.8834 http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.8834 http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf Thematic Cartography Glacier Mapping Glacier Motion Glacier Rheology Differential SAR Interferometry Crevasse-Danger Map Svartisen Ice Caps Hintereis Glacier text ftciteseerx 2016-01-08T10:41:29Z Abstract: In cooperation between remote sensing experts and cartographers interested in glaciology new types of maps showing the glacier dynamics have been developed. The map make use of the original phase gradient approach to glacier rheology modelling based on repeat-pass ERTS SAR interferograms. Careful map design and, in particular, colour assignment allow the visualization of the glacier dynamics in its locally changing velocity with an estimated accuracy of approx. 2.0 cm per day. In fact, two map derivates, a differential interferogram showing the glacier velocity and another product displaying the glacier strain rate, have been designed. Moreover, maps displaying the glacier marginal changes within four years have generated. The strain rate maps evidenced that spots with high values frequently correspond with crevasse-prone areas which can even be detected under thick layers of snow. In this sense, the latter visualizations can be seen as a sort of maps of crevasse-danger zones. The Svartisen Ice Caps in Norway and the Hintereis Glacier in Austria served as Text glacier Svartisen Unknown Norway Svartisen ENVELOPE(13.698,13.698,66.642,66.642)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Thematic Cartography
Glacier Mapping
Glacier Motion
Glacier Rheology
Differential SAR Interferometry
Crevasse-Danger Map
Svartisen Ice Caps
Hintereis Glacier
spellingShingle Thematic Cartography
Glacier Mapping
Glacier Motion
Glacier Rheology
Differential SAR Interferometry
Crevasse-Danger Map
Svartisen Ice Caps
Hintereis Glacier
Manfred F. Buchroithner
Sebastian Walther
DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
topic_facet Thematic Cartography
Glacier Mapping
Glacier Motion
Glacier Rheology
Differential SAR Interferometry
Crevasse-Danger Map
Svartisen Ice Caps
Hintereis Glacier
description Abstract: In cooperation between remote sensing experts and cartographers interested in glaciology new types of maps showing the glacier dynamics have been developed. The map make use of the original phase gradient approach to glacier rheology modelling based on repeat-pass ERTS SAR interferograms. Careful map design and, in particular, colour assignment allow the visualization of the glacier dynamics in its locally changing velocity with an estimated accuracy of approx. 2.0 cm per day. In fact, two map derivates, a differential interferogram showing the glacier velocity and another product displaying the glacier strain rate, have been designed. Moreover, maps displaying the glacier marginal changes within four years have generated. The strain rate maps evidenced that spots with high values frequently correspond with crevasse-prone areas which can even be detected under thick layers of snow. In this sense, the latter visualizations can be seen as a sort of maps of crevasse-danger zones. The Svartisen Ice Caps in Norway and the Hintereis Glacier in Austria served as
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Manfred F. Buchroithner
Sebastian Walther
author_facet Manfred F. Buchroithner
Sebastian Walther
author_sort Manfred F. Buchroithner
title DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
title_short DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
title_full DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
title_fullStr DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
title_full_unstemmed DEVELOPMENT OF NEW TYPES OF GLACIER DYNAMICS MAPS
title_sort development of new types of glacier dynamics maps
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.8834
http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf
long_lat ENVELOPE(13.698,13.698,66.642,66.642)
geographic Norway
Svartisen
geographic_facet Norway
Svartisen
genre glacier
Svartisen
genre_facet glacier
Svartisen
op_source http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.8834
http://www.mountaincartography.org/publications/papers/papers_bohinj_06/02_Buchroithner.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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