Layer optimized SAR processing and slope estimation in radar sounder data
Englacial layers in Antarctica and Greenland are indicators of the dynamic, rheological and subglacial configuration of the ice sheets. Airborne radar sounder data is the primary remote sensing solution for directly observing englacial layers and structures at the glacier-catchment to ice-sheet scal...
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Cambridge University Press
2019
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Online Access: | https://doi.org/10.1017/jog.2019.72 https://doaj.org/article/937b12754570474481a6dca5d27481ba |
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ftdoajarticles:oai:doaj.org/article:937b12754570474481a6dca5d27481ba 2023-05-15T13:47:33+02:00 Layer optimized SAR processing and slope estimation in radar sounder data Davide Castelletti Dustin M. Schroeder Elisa Mantelli Andrew Hilger 2019-12-01T00:00:00Z https://doi.org/10.1017/jog.2019.72 https://doaj.org/article/937b12754570474481a6dca5d27481ba EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143019000728/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2019.72 0022-1430 1727-5652 https://doaj.org/article/937b12754570474481a6dca5d27481ba Journal of Glaciology, Vol 65, Pp 983-988 (2019) Radio-echo sounding ice dynamics remote sensing Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2019 ftdoajarticles https://doi.org/10.1017/jog.2019.72 2023-03-12T01:30:57Z Englacial layers in Antarctica and Greenland are indicators of the dynamic, rheological and subglacial configuration of the ice sheets. Airborne radar sounder data is the primary remote sensing solution for directly observing englacial layers and structures at the glacier-catchment to ice-sheet scale. However, when traditional along-track synthetic aperture radar (SAR) processing is applied, steep layers can disappear, limiting the detectability and interpretability of englacial layer geometry. This study provides a reconstruction algorithm to address the problem of destructive phase interference during the radargram formation. We develop and apply a novel SAR processor optimized for layer detection that enhances the Signal-to-Noise ratio (SNR) of specular reflectors. The algorithm also enables the automatic estimation of layer slope. We demonstrate the algorithm using data acquired at the Institute Ice Stream, West Antarctica. Article in Journal/Newspaper Antarc* Antarctica glacier Greenland Ice Sheet Institute Ice Stream Journal of Glaciology West Antarctica Directory of Open Access Journals: DOAJ Articles West Antarctica Greenland Institute Ice Stream ENVELOPE(-75.000,-75.000,-82.000,-82.000) Journal of Glaciology 65 254 983 988 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Radio-echo sounding ice dynamics remote sensing Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Radio-echo sounding ice dynamics remote sensing Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Davide Castelletti Dustin M. Schroeder Elisa Mantelli Andrew Hilger Layer optimized SAR processing and slope estimation in radar sounder data |
topic_facet |
Radio-echo sounding ice dynamics remote sensing Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Englacial layers in Antarctica and Greenland are indicators of the dynamic, rheological and subglacial configuration of the ice sheets. Airborne radar sounder data is the primary remote sensing solution for directly observing englacial layers and structures at the glacier-catchment to ice-sheet scale. However, when traditional along-track synthetic aperture radar (SAR) processing is applied, steep layers can disappear, limiting the detectability and interpretability of englacial layer geometry. This study provides a reconstruction algorithm to address the problem of destructive phase interference during the radargram formation. We develop and apply a novel SAR processor optimized for layer detection that enhances the Signal-to-Noise ratio (SNR) of specular reflectors. The algorithm also enables the automatic estimation of layer slope. We demonstrate the algorithm using data acquired at the Institute Ice Stream, West Antarctica. |
format |
Article in Journal/Newspaper |
author |
Davide Castelletti Dustin M. Schroeder Elisa Mantelli Andrew Hilger |
author_facet |
Davide Castelletti Dustin M. Schroeder Elisa Mantelli Andrew Hilger |
author_sort |
Davide Castelletti |
title |
Layer optimized SAR processing and slope estimation in radar sounder data |
title_short |
Layer optimized SAR processing and slope estimation in radar sounder data |
title_full |
Layer optimized SAR processing and slope estimation in radar sounder data |
title_fullStr |
Layer optimized SAR processing and slope estimation in radar sounder data |
title_full_unstemmed |
Layer optimized SAR processing and slope estimation in radar sounder data |
title_sort |
layer optimized sar processing and slope estimation in radar sounder data |
publisher |
Cambridge University Press |
publishDate |
2019 |
url |
https://doi.org/10.1017/jog.2019.72 https://doaj.org/article/937b12754570474481a6dca5d27481ba |
long_lat |
ENVELOPE(-75.000,-75.000,-82.000,-82.000) |
geographic |
West Antarctica Greenland Institute Ice Stream |
geographic_facet |
West Antarctica Greenland Institute Ice Stream |
genre |
Antarc* Antarctica glacier Greenland Ice Sheet Institute Ice Stream Journal of Glaciology West Antarctica |
genre_facet |
Antarc* Antarctica glacier Greenland Ice Sheet Institute Ice Stream Journal of Glaciology West Antarctica |
op_source |
Journal of Glaciology, Vol 65, Pp 983-988 (2019) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143019000728/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2019.72 0022-1430 1727-5652 https://doaj.org/article/937b12754570474481a6dca5d27481ba |
op_doi |
https://doi.org/10.1017/jog.2019.72 |
container_title |
Journal of Glaciology |
container_volume |
65 |
container_issue |
254 |
container_start_page |
983 |
op_container_end_page |
988 |
_version_ |
1766247290452836352 |