Cryosat-2 Interferometric SAR Altimetry

Cryosat-2 altimetry helps to assess the state of the Cryosphere by measuring elevation and elevation change. The SARIn mode of the Cryosat-2 SIRAL instrument is specifically designed for rough topography that we encounter near ice sheet margins. Various SARIn data products (Full Bit Rate (FBR), Leve...

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Bibliographic Details
Main Author: Verhoeven, Corné (author)
Other Authors: Schrama, Ernst (mentor), Delft University of Technology (degree granting institution)
Format: Bachelor Thesis
Language:English
Published: 2018
Subjects:
SAR
Ice
Online Access:http://resolver.tudelft.nl/uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37
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record_format openpolar
spelling fttudelft:oai:tudelft.nl:uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37 2023-07-30T04:03:37+02:00 Cryosat-2 Interferometric SAR Altimetry Verhoeven, Corné (author) Schrama, Ernst (mentor) Delft University of Technology (degree granting institution) 2018-12-21 http://resolver.tudelft.nl/uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37 en eng http://resolver.tudelft.nl/uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37 © 2018 Corné Verhoeven Altimetry SAR Radar Signal Processing Swath Ice Petermann Glacier bachelor thesis 2018 fttudelft 2023-07-08T20:31:12Z Cryosat-2 altimetry helps to assess the state of the Cryosphere by measuring elevation and elevation change. The SARIn mode of the Cryosat-2 SIRAL instrument is specifically designed for rough topography that we encounter near ice sheet margins. Various SARIn data products (Full Bit Rate (FBR), Level 1b and Level 2) are provided by ESA, where the level denotes the amount of processing applied relative to the raw instrument data. Often research activities are based on L1b data; in this thesis, a new Cryosat-2 SARIn FBR-to-L1b processor is developed to evaluate whether elevation measurements improve when we reconstruct a L1b product from the FBR data. The L1b-to-L2 processing is performed by means of Swath Processing, by which an increase in amount of measurement points is achieved with respect to the amount in conventional L2 products. The analysis is limited to the Petermann glacier, located in the North-West of Greenland, which is known for its large calving events. The results are verified by comparing them to the ESA products. It is shown that the resulting elevations following from the FBR-to-L1b processor agree; we detect significant variability in topography as present in the Petermann Glacier region that can induce data gaps in the raw FBR data; with consequences for the L1b- and L2 products. Overall, it is shown that small improvements in terms of accuracy can be achieved with respect to the ESA L1b data; this conclusion follows from the consideration of independent IceBridge laser altimetry data in our study. Aerospace Engineering | Space Exploration Bachelor Thesis glacier Greenland Ice Sheet Petermann glacier Delft University of Technology: Institutional Repository Greenland
institution Open Polar
collection Delft University of Technology: Institutional Repository
op_collection_id fttudelft
language English
topic Altimetry
SAR
Radar
Signal Processing
Swath
Ice
Petermann Glacier
spellingShingle Altimetry
SAR
Radar
Signal Processing
Swath
Ice
Petermann Glacier
Verhoeven, Corné (author)
Cryosat-2 Interferometric SAR Altimetry
topic_facet Altimetry
SAR
Radar
Signal Processing
Swath
Ice
Petermann Glacier
description Cryosat-2 altimetry helps to assess the state of the Cryosphere by measuring elevation and elevation change. The SARIn mode of the Cryosat-2 SIRAL instrument is specifically designed for rough topography that we encounter near ice sheet margins. Various SARIn data products (Full Bit Rate (FBR), Level 1b and Level 2) are provided by ESA, where the level denotes the amount of processing applied relative to the raw instrument data. Often research activities are based on L1b data; in this thesis, a new Cryosat-2 SARIn FBR-to-L1b processor is developed to evaluate whether elevation measurements improve when we reconstruct a L1b product from the FBR data. The L1b-to-L2 processing is performed by means of Swath Processing, by which an increase in amount of measurement points is achieved with respect to the amount in conventional L2 products. The analysis is limited to the Petermann glacier, located in the North-West of Greenland, which is known for its large calving events. The results are verified by comparing them to the ESA products. It is shown that the resulting elevations following from the FBR-to-L1b processor agree; we detect significant variability in topography as present in the Petermann Glacier region that can induce data gaps in the raw FBR data; with consequences for the L1b- and L2 products. Overall, it is shown that small improvements in terms of accuracy can be achieved with respect to the ESA L1b data; this conclusion follows from the consideration of independent IceBridge laser altimetry data in our study. Aerospace Engineering | Space Exploration
author2 Schrama, Ernst (mentor)
Delft University of Technology (degree granting institution)
format Bachelor Thesis
author Verhoeven, Corné (author)
author_facet Verhoeven, Corné (author)
author_sort Verhoeven, Corné (author)
title Cryosat-2 Interferometric SAR Altimetry
title_short Cryosat-2 Interferometric SAR Altimetry
title_full Cryosat-2 Interferometric SAR Altimetry
title_fullStr Cryosat-2 Interferometric SAR Altimetry
title_full_unstemmed Cryosat-2 Interferometric SAR Altimetry
title_sort cryosat-2 interferometric sar altimetry
publishDate 2018
url http://resolver.tudelft.nl/uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
Ice Sheet
Petermann glacier
genre_facet glacier
Greenland
Ice Sheet
Petermann glacier
op_relation http://resolver.tudelft.nl/uuid:42467c49-06eb-4421-89ca-6dcc41ff6e37
op_rights © 2018 Corné Verhoeven
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