Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change

There are an increasing number of digital elevation models (DEMs) available worldwide for deriving elevation differences over time, including vertical changes on glaciers. Most of these DEMs are heavily post-processed or merged, so that physical error modelling becomes difficult and statistical erro...

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Published in:The Cryosphere
Main Authors: C. Nuth, A. Kääb
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/tc-5-271-2011
https://doaj.org/article/e3fd08ed60694cb4b68f091ebe531e6c
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spelling ftdoajarticles:oai:doaj.org/article:e3fd08ed60694cb4b68f091ebe531e6c 2023-05-15T16:22:16+02:00 Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change C. Nuth A. Kääb 2011-03-01T00:00:00Z https://doi.org/10.5194/tc-5-271-2011 https://doaj.org/article/e3fd08ed60694cb4b68f091ebe531e6c EN eng Copernicus Publications http://www.the-cryosphere.net/5/271/2011/tc-5-271-2011.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-5-271-2011 1994-0416 1994-0424 https://doaj.org/article/e3fd08ed60694cb4b68f091ebe531e6c The Cryosphere, Vol 5, Iss 1, Pp 271-290 (2011) Environmental sciences GE1-350 Geology QE1-996.5 article 2011 ftdoajarticles https://doi.org/10.5194/tc-5-271-2011 2022-12-31T14:57:25Z There are an increasing number of digital elevation models (DEMs) available worldwide for deriving elevation differences over time, including vertical changes on glaciers. Most of these DEMs are heavily post-processed or merged, so that physical error modelling becomes difficult and statistical error modelling is required instead. We propose a three-step methodological framework for assessing and correcting DEMs to quantify glacier elevation changes: (i) remove DEM shifts, (ii) check for elevation-dependent biases, and (iii) check for higher-order, sensor-specific biases. A simple, analytic and robust method to co-register elevation data is presented in regions where stable terrain is either plentiful (case study New Zealand) or limited (case study Svalbard). The method is demonstrated using the three global elevation data sets available to date, SRTM, ICESat and the ASTER GDEM, and with automatically generated DEMs from satellite stereo instruments of ASTER and SPOT5-HRS. After 3-D co-registration, significant biases related to elevation were found in some of the stereoscopic DEMs. Biases related to the satellite acquisition geometry (along/cross track) were detected at two frequencies in the automatically generated ASTER DEMs. The higher frequency bias seems to be related to satellite jitter , most apparent in the back-looking pass of the satellite. The origins of the more significant lower frequency bias is uncertain. ICESat-derived elevations are found to be the most consistent globally available elevation data set available so far. Before performing regional-scale glacier elevation change studies or mosaicking DEMs from multiple individual tiles (e.g. ASTER GDEM), we recommend to co-register all elevation data to ICESat as a global vertical reference system. Article in Journal/Newspaper glacier Svalbard The Cryosphere Directory of Open Access Journals: DOAJ Articles New Zealand Svalbard The Cryosphere 5 1 271 290
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
C. Nuth
A. Kääb
Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description There are an increasing number of digital elevation models (DEMs) available worldwide for deriving elevation differences over time, including vertical changes on glaciers. Most of these DEMs are heavily post-processed or merged, so that physical error modelling becomes difficult and statistical error modelling is required instead. We propose a three-step methodological framework for assessing and correcting DEMs to quantify glacier elevation changes: (i) remove DEM shifts, (ii) check for elevation-dependent biases, and (iii) check for higher-order, sensor-specific biases. A simple, analytic and robust method to co-register elevation data is presented in regions where stable terrain is either plentiful (case study New Zealand) or limited (case study Svalbard). The method is demonstrated using the three global elevation data sets available to date, SRTM, ICESat and the ASTER GDEM, and with automatically generated DEMs from satellite stereo instruments of ASTER and SPOT5-HRS. After 3-D co-registration, significant biases related to elevation were found in some of the stereoscopic DEMs. Biases related to the satellite acquisition geometry (along/cross track) were detected at two frequencies in the automatically generated ASTER DEMs. The higher frequency bias seems to be related to satellite jitter , most apparent in the back-looking pass of the satellite. The origins of the more significant lower frequency bias is uncertain. ICESat-derived elevations are found to be the most consistent globally available elevation data set available so far. Before performing regional-scale glacier elevation change studies or mosaicking DEMs from multiple individual tiles (e.g. ASTER GDEM), we recommend to co-register all elevation data to ICESat as a global vertical reference system.
format Article in Journal/Newspaper
author C. Nuth
A. Kääb
author_facet C. Nuth
A. Kääb
author_sort C. Nuth
title Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
title_short Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
title_full Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
title_fullStr Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
title_full_unstemmed Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
title_sort co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/tc-5-271-2011
https://doaj.org/article/e3fd08ed60694cb4b68f091ebe531e6c
geographic New Zealand
Svalbard
geographic_facet New Zealand
Svalbard
genre glacier
Svalbard
The Cryosphere
genre_facet glacier
Svalbard
The Cryosphere
op_source The Cryosphere, Vol 5, Iss 1, Pp 271-290 (2011)
op_relation http://www.the-cryosphere.net/5/271/2011/tc-5-271-2011.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-5-271-2011
1994-0416
1994-0424
https://doaj.org/article/e3fd08ed60694cb4b68f091ebe531e6c
op_doi https://doi.org/10.5194/tc-5-271-2011
container_title The Cryosphere
container_volume 5
container_issue 1
container_start_page 271
op_container_end_page 290
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