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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Main Authors: M. Scaioni, X. Tong, R. Li
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-5-W2/253/2013/isprsannals-II-5-W2-253-2013.pdf
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spelling 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
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