USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON
Multi-year SAR data is used to study the seasonal dynamic of the snow melt patterns on the ice cap of King George Island, Antarctica. The snow cover of the entire ice cap becomes wet during sum-mer months, however, in the highest elevations frequent refreeze and melt cycles are observed. Bare ice ar...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.522.657 2023-05-15T13:39:32+02:00 USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON Matthias Braun Frank Rau The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.522.657 http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.522.657 http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf text ftciteseerx 2016-01-08T10:12:59Z Multi-year SAR data is used to study the seasonal dynamic of the snow melt patterns on the ice cap of King George Island, Antarctica. The snow cover of the entire ice cap becomes wet during sum-mer months, however, in the highest elevations frequent refreeze and melt cycles are observed. Bare ice areas form in the lowest elevations of the ice cap. These findings are in good agreements with energy balance studies and results of a ground penetrating radar survey. Backscatter values in in-termediate elevations show a marked rise at the end of the ablation season. This fact is attributed to an increasing surface roughness on a wet metamorphosed snow cover at the end of the ablation sea-son. The influence of thresholds on the determination of the extent of the bare ice radar zone in summer and winter imagery as well as in ascending and descending orbit is investigated. As a con-sequence, the border of the bare ice radar zone have been mapped using thresholds of –14 dB in summer and –6 dB in winter imagery. It could be shown, that thresholds of –12 dB and –8 dB, re-spectively, do not change significantly the extent of this radar glacier zone. Firn line altitudes were mapped for several consecutive years. A low inter-annual variation of this line with elevations of about 200 m a.s.l. was observed. The maximum altitude of the firn line was recorded in the mass balance year 1996/97with about 250 m a.s.l. Comparing these values to equilibrium line positions of previous measurements indicate an upward shift in the equilibrium line altitude since the 1970’s. Text Antarc* Antarctica Ice cap King George Island Unknown King George Island |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Multi-year SAR data is used to study the seasonal dynamic of the snow melt patterns on the ice cap of King George Island, Antarctica. The snow cover of the entire ice cap becomes wet during sum-mer months, however, in the highest elevations frequent refreeze and melt cycles are observed. Bare ice areas form in the lowest elevations of the ice cap. These findings are in good agreements with energy balance studies and results of a ground penetrating radar survey. Backscatter values in in-termediate elevations show a marked rise at the end of the ablation season. This fact is attributed to an increasing surface roughness on a wet metamorphosed snow cover at the end of the ablation sea-son. The influence of thresholds on the determination of the extent of the bare ice radar zone in summer and winter imagery as well as in ascending and descending orbit is investigated. As a con-sequence, the border of the bare ice radar zone have been mapped using thresholds of –14 dB in summer and –6 dB in winter imagery. It could be shown, that thresholds of –12 dB and –8 dB, re-spectively, do not change significantly the extent of this radar glacier zone. Firn line altitudes were mapped for several consecutive years. A low inter-annual variation of this line with elevations of about 200 m a.s.l. was observed. The maximum altitude of the firn line was recorded in the mass balance year 1996/97with about 250 m a.s.l. Comparing these values to equilibrium line positions of previous measurements indicate an upward shift in the equilibrium line altitude since the 1970’s. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Matthias Braun Frank Rau |
spellingShingle |
Matthias Braun Frank Rau USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
author_facet |
Matthias Braun Frank Rau |
author_sort |
Matthias Braun |
title |
USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
title_short |
USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
title_full |
USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
title_fullStr |
USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
title_full_unstemmed |
USING A MULTI-YEAR DATA ARCHIVE OF ERS SAR IMAGERY FOR THE MONITORING OF FIRN LINE POSITIONS AND ABLATION PATTERNS ON |
title_sort |
using a multi-year data archive of ers sar imagery for the monitoring of firn line positions and ablation patterns on |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.522.657 http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf |
geographic |
King George Island |
geographic_facet |
King George Island |
genre |
Antarc* Antarctica Ice cap King George Island |
genre_facet |
Antarc* Antarctica Ice cap King George Island |
op_source |
http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.522.657 http://las.physik.uni-oldenburg.de/eProceedings/vol01_1/01_1_braun1.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766120030566612992 |