Application of glas laser altimetry to detect elevation changes in East Antarctica
In this paper the use of ICESat/GLAS laser altimeter for estimating multi-temporal elevation changes on polar ice sheets is afforded. Due to non-overlapping laser spots during repeat passes, interpolation methods are required to make comparisons. After reviewing the main methods described in the l...
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doaj-c1756a88efc7440c92ea27639d7da2ff2020-11-25T01:39:11ZengCopernicus PublicationsISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences2194-90422194-90502013-10-01II-5-W225325810.5194/isprsannals-II-5-W2-253-2013Application of glas laser altimetry to detect elevation changes in East AntarcticaM. Scaioni0X. Tong1R. Li2R. Li3Tongji University, College of Surveying and Geo-Informatics Center for Spatial Information Science and Sustainable Development Applications 1239 Siping Road, 200092 Shanghai, P. R. ChinaTongji University, College of Surveying and Geo-Informatics Center for Spatial Information Science and Sustainable Development Applications 1239 Siping Road, 200092 Shanghai, P. R. ChinaThe Ohio State University, Mapping and GIS Lab 470 Hitchcock Hall, 2070 Neil Avenue, Columbus, OH 43210-1275, USATongji University, College of Surveying and Geo-Informatics Center for Spatial Information Science and Sustainable Development Applications 1239 Siping Road, 200092 Shanghai, P. R. ChinaIn this paper the use of ICESat/GLAS laser altimeter for estimating multi-temporal elevation changes on polar ice sheets is afforded. Due to non-overlapping laser spots during repeat passes, interpolation methods are required to make comparisons. After reviewing the main methods described in the literature (<i>crossover point analysis, cross-track DEM projection, space-temporal regressions</i>), the last one has been chosen for its capability of providing more elevation change rate measurements. The standard implementation of the <i>space-temporal linear regression</i> technique has been revisited and improved to better cope with outliers and to check the estimability of model’s parameters. GLAS data over the PANDA route in East Antarctica have been used for testing. Obtained results have been quite meaningful from a physical point of view, confirming the trend reported by the literature of a constant snow accumulation in the area during the two past decades, unlike the most part of the continent that has been losing mass.https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-5-W2/253/2013/isprsannals-II-5-W2-253-2013.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
M. Scaioni X. Tong R. Li R. Li |
spellingShingle |
M. Scaioni X. Tong R. Li R. Li Application of glas laser altimetry to detect elevation changes in East Antarctica ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences |
author_facet |
M. Scaioni X. Tong R. Li R. Li |
author_sort |
M. Scaioni |
title |
Application of glas laser altimetry to detect elevation changes in East Antarctica |
title_short |
Application of glas laser altimetry to detect elevation changes in East Antarctica |
title_full |
Application of glas laser altimetry to detect elevation changes in East Antarctica |
title_fullStr |
Application of glas laser altimetry to detect elevation changes in East Antarctica |
title_full_unstemmed |
Application of glas laser altimetry to detect elevation changes in East Antarctica |
title_sort |
application of glas laser altimetry to detect elevation changes in east antarctica |
publisher |
Copernicus Publications |
series |
ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences |
issn |
2194-9042 2194-9050 |
publishDate |
2013-10-01 |
description |
In this paper the use of ICESat/GLAS laser altimeter for estimating multi-temporal elevation changes on polar ice sheets is afforded.
Due to non-overlapping laser spots during repeat passes, interpolation methods are required to make comparisons. After reviewing
the main methods described in the literature (<i>crossover point analysis, cross-track DEM projection, space-temporal regressions</i>), the
last one has been chosen for its capability of providing more elevation change rate measurements. The standard implementation of
the <i>space-temporal linear regression</i> technique has been revisited and improved to better cope with outliers and to check the
estimability of model’s parameters. GLAS data over the PANDA route in East Antarctica have been used for testing. Obtained
results have been quite meaningful from a physical point of view, confirming the trend reported by the literature of a constant snow
accumulation in the area during the two past decades, unlike the most part of the continent that has been losing mass. |
url |
https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-5-W2/253/2013/isprsannals-II-5-W2-253-2013.pdf |
work_keys_str_mv |
AT mscaioni applicationofglaslaseraltimetrytodetectelevationchangesineastantarctica AT xtong applicationofglaslaseraltimetrytodetectelevationchangesineastantarctica AT rli applicationofglaslaseraltimetrytodetectelevationchangesineastantarctica AT rli applicationofglaslaseraltimetrytodetectelevationchangesineastantarctica |
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