Coastal sea level from inland CryoSat-2 interferometric SAR altimetry

The European Space Agency's CryoSat-2 satellite can operate in a novel synthetic aperture radar interferometric (SARIn) mode where its nominal footprint (swath) is observed by two antennas and the phase difference between the signals is used to determination the exact location of the scatterer...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Abulaitijiang, Adili, Andersen, Ole Baltazar, Stenseng, Lars
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/8310aea1-49b4-4483-b791-a6236a09745f
https://doi.org/10.1002/2015GL063131
id ftdtupubl:oai:pure.atira.dk:publications/8310aea1-49b4-4483-b791-a6236a09745f
record_format openpolar
spelling ftdtupubl:oai:pure.atira.dk:publications/8310aea1-49b4-4483-b791-a6236a09745f 2024-05-19T07:41:21+00:00 Coastal sea level from inland CryoSat-2 interferometric SAR altimetry Abulaitijiang, Adili Andersen, Ole Baltazar Stenseng, Lars 2015 https://orbit.dtu.dk/en/publications/8310aea1-49b4-4483-b791-a6236a09745f https://doi.org/10.1002/2015GL063131 eng eng https://orbit.dtu.dk/en/publications/8310aea1-49b4-4483-b791-a6236a09745f info:eu-repo/semantics/closedAccess Abulaitijiang , A , Andersen , O B & Stenseng , L 2015 , ' Coastal sea level from inland CryoSat-2 interferometric SAR altimetry ' , Geophysical Research Letters , vol. 42 , no. 6 , pp. 1841-1847 . https://doi.org/10.1002/2015GL063131 Altimetry SAR interferometry Interferometry Satellites Space-based radar Synthetic aperture radar Coastal sea level European Space Agency Interferometric SAR Phase difference Phase wrapping Track direction Sea level article 2015 ftdtupubl https://doi.org/10.1002/2015GL063131 2024-05-01T00:21:07Z The European Space Agency's CryoSat-2 satellite can operate in a novel synthetic aperture radar interferometric (SARIn) mode where its nominal footprint (swath) is observed by two antennas and the phase difference between the signals is used to determination the exact location of the scatterer through an off-nadir correction. The potential of SARIn for sea level determination is investigated over the fjords of Eastern Greenland. In principle the satellite should only track sea level within its nominal footprint of 7km across track, but we observe that scattering targets (fjords) within twice its nominal footprint are frequently observed but mislocated in CryoSat-2 due to phase wrapping. We devised a way to relocate the observations and correct the range accordingly. When CryoSat-2 is flying inland we consequently observed that the satellite occasionally provide valid sea level in fjords up to 13km away in the across-track direction. Article in Journal/Newspaper Greenland Technical University of Denmark: DTU Orbit Geophysical Research Letters 42 6 1841 1847
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
topic Altimetry
SAR interferometry
Interferometry
Satellites
Space-based radar
Synthetic aperture radar
Coastal sea level
European Space Agency
Interferometric SAR
Phase difference
Phase wrapping
Track direction
Sea level
spellingShingle Altimetry
SAR interferometry
Interferometry
Satellites
Space-based radar
Synthetic aperture radar
Coastal sea level
European Space Agency
Interferometric SAR
Phase difference
Phase wrapping
Track direction
Sea level
Abulaitijiang, Adili
Andersen, Ole Baltazar
Stenseng, Lars
Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
topic_facet Altimetry
SAR interferometry
Interferometry
Satellites
Space-based radar
Synthetic aperture radar
Coastal sea level
European Space Agency
Interferometric SAR
Phase difference
Phase wrapping
Track direction
Sea level
description The European Space Agency's CryoSat-2 satellite can operate in a novel synthetic aperture radar interferometric (SARIn) mode where its nominal footprint (swath) is observed by two antennas and the phase difference between the signals is used to determination the exact location of the scatterer through an off-nadir correction. The potential of SARIn for sea level determination is investigated over the fjords of Eastern Greenland. In principle the satellite should only track sea level within its nominal footprint of 7km across track, but we observe that scattering targets (fjords) within twice its nominal footprint are frequently observed but mislocated in CryoSat-2 due to phase wrapping. We devised a way to relocate the observations and correct the range accordingly. When CryoSat-2 is flying inland we consequently observed that the satellite occasionally provide valid sea level in fjords up to 13km away in the across-track direction.
format Article in Journal/Newspaper
author Abulaitijiang, Adili
Andersen, Ole Baltazar
Stenseng, Lars
author_facet Abulaitijiang, Adili
Andersen, Ole Baltazar
Stenseng, Lars
author_sort Abulaitijiang, Adili
title Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
title_short Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
title_full Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
title_fullStr Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
title_full_unstemmed Coastal sea level from inland CryoSat-2 interferometric SAR altimetry
title_sort coastal sea level from inland cryosat-2 interferometric sar altimetry
publishDate 2015
url https://orbit.dtu.dk/en/publications/8310aea1-49b4-4483-b791-a6236a09745f
https://doi.org/10.1002/2015GL063131
genre Greenland
genre_facet Greenland
op_source Abulaitijiang , A , Andersen , O B & Stenseng , L 2015 , ' Coastal sea level from inland CryoSat-2 interferometric SAR altimetry ' , Geophysical Research Letters , vol. 42 , no. 6 , pp. 1841-1847 . https://doi.org/10.1002/2015GL063131
op_relation https://orbit.dtu.dk/en/publications/8310aea1-49b4-4483-b791-a6236a09745f
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1002/2015GL063131
container_title Geophysical Research Letters
container_volume 42
container_issue 6
container_start_page 1841
op_container_end_page 1847
_version_ 1799480955003469824