A new digital elevation model (DEM) dataset of the entire Antarctic continent derived from ICESat-2
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Published:2022-07-06
Issue:7
Volume:14
Page:3075-3089
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ISSN:1866-3516
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Container-title:Earth System Science Data
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language:en
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Short-container-title:Earth Syst. Sci. Data
Author:
Shen Xiaoyi,Ke Chang-Qing,Fan Yubin,Drolma Lhakpa
Abstract
Abstract. Antarctic digital elevation models (DEMs) are essential
for fieldwork, ice motion tracking and the numerical modelling of the ice sheet.
In the past 30 years, several Antarctic DEMs derived from satellite data
have been published. However, these DEMs either have coarse spatial
resolution or aggregate observations spanning several years, which
limit their further scientific applications. In this study, the
new generation satellite laser altimeter Ice, Cloud, and Land Elevation
Satellite-2 (ICESat-2) is used to generate a new Antarctic DEM for both the
ice sheet and ice shelves. Approximately 4.69 × 109 ICESat-2
measurement points from November 2018 to November 2019 are used to estimate
surface elevations at resolutions of 500 m and 1 km based on a
spatiotemporal fitting method. Approximately 74 % of Antarctica is
observed and the remaining observation gaps are interpolated using the
normal kriging method. The DEM is formed from the estimated elevations in
500 m and 1 km grid cells, and is finally posted at the resolution of 500 m.
National Aeronautics and Space Administration (NASA) Operation IceBridge (OIB)
airborne data are used to evaluate the generated Antarctic DEM (hereafter
called the ICESat-2 DEM) in individual Antarctic regions and surface types.
Overall, a median bias of −0.19 m and a root-mean-square deviation of 10.83
m result from approximately 5.2 × 106 OIB measurement
points. The accuracy and uncertainty of the ICESat-2 DEM vary in relation to
the surface slope and roughness, and more reliable estimates are found in
the flat ice sheet interior. The ICESat-2 DEM is comparable to other DEMs
derived from altimetry, stereophotogrammetry and interferometry. Similar
results are found when comparing to elevation measurements from kinematic Global Navigation Satellite System
(GNSS) (GPS and the Russian GLONASS) transects. The elevations of high
accuracy and ability of annual updates make the ICESat-2 DEM an addition to
the existing Antarctic DEM groups, and it can be further used for other
scientific applications. The generated ICESat-2 DEM (including the map of
uncertainty) can be downloaded from National Tibetan Plateau Data Center,
Institute of Tibetan Plateau Research, Chinese Academy of Sciences at
https://data.tpdc.ac.cn/en/disallow/9427069c-117e-4ff8-96e0-4b18eb7782cb/ (last access: 27 June 2022)
(Shen et al., 2021a, https://doi.org/10.11888/Geogra.tpdc.271448).
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
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