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Development of an Antarctic digital elevation model by integrating cartographic and remotely sensed data: A geographic information system based approach

We present a high‐resolution digital elevation model (DEM) of the Antarctic. It was created in a geographic information system (GIS) environment by integrating the best available topographic data from a variety of sources. Extensive GIS‐based error detection and correction operations ensured that ou...

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Published in:Journal of Geophysical Research 1999-10, Vol.104 (B10), p.23199-23213
Main Authors: Liu, Hongxing, Jezek, Kenneth C., Li, Biyan
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Language:English
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cited_by cdi_FETCH-LOGICAL-a5029-8d9d33212ede1336f6ffed5977140ea09a1c7ad5b4b871fc9056082b2eceb1953
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container_end_page 23213
container_issue B10
container_start_page 23199
container_title Journal of Geophysical Research
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creator Liu, Hongxing
Jezek, Kenneth C.
Li, Biyan
description We present a high‐resolution digital elevation model (DEM) of the Antarctic. It was created in a geographic information system (GIS) environment by integrating the best available topographic data from a variety of sources. Extensive GIS‐based error detection and correction operations ensured that our DEM is free of gross errors. The carefully designed interpolation algorithms for different types of source data and incorporation of surface morphologic information preserved and enhanced the fine surface structures present in the source data. The effective control of adverse edge effects and the use of the Hermite blending weight function in data merging minimized the discontinuities between different types of data, leading to a seamless and topographically consistent DEM throughout the Antarctic. This new DEM provides exceptional topographical details and represents a substantial improvement in horizontal resolution and vertical accuracy over the earlier, continental‐scale renditions, particularly in mountainous and coastal regions. It has a horizontal resolution of 200 m over the rugged mountains, 400 m in the coastal regions, and approximately 5 km in the interior. The vertical accuracy of the DEM is estimated at about 100–130 m over the rugged mountainous area, better than 2 m for the ice shelves, better than 15 m for the interior ice sheet, and about 35 m for the steeper ice sheet perimeter. The Antarctic DEM can be obtained from the authors.
doi_str_mv 10.1029/1999JB900224
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source Wiley-Blackwell AGU Digital Archive
subjects Applied geophysics
Earth sciences
Earth, ocean, space
Exact sciences and technology
Internal geophysics
Solid-earth geophysics, tectonophysics, gravimetry
title Development of an Antarctic digital elevation model by integrating cartographic and remotely sensed data: A geographic information system based approach
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