Assessment of ASTER global digital elevation model data for Arctic research
ABSTRACT A new source of digital elevation data, the advanced spaceborne thermal emission and reflection radiometer (ASTER) global digital elevation model (GDEM), has been freely available since 2009. It provides enormously greater coverage of the Arctic than previous satellite derived ‘global’ digi...
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crcambridgeupr:10.1017/s0032247411000325 2024-03-03T08:41:33+00:00 Assessment of ASTER global digital elevation model data for Arctic research Rees, W. G. 2011 http://dx.doi.org/10.1017/s0032247411000325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247411000325 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 48, issue 1, page 31-39 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 2011 crcambridgeupr https://doi.org/10.1017/s0032247411000325 2024-02-08T08:31:52Z ABSTRACT A new source of digital elevation data, the advanced spaceborne thermal emission and reflection radiometer (ASTER) global digital elevation model (GDEM), has been freely available since 2009. It provides enormously greater coverage of the Arctic than previous satellite derived ‘global’ digital elevation models, extending to a latitude of 83 °N in contrast to 60 °N. The GDEM is described as a preliminary, research grade product. This paper investigates its accuracy in a number of specifically Arctic landscapes, including ice and snow, boreal forest, tundra and unvegetated terrain, using test sites in Svalbard, Iceland, Norway and Russia. Semivariogram analysis is used to characterise the magnitude and spatial correlation of errors in the GDEM products from the test sites. The analysis suggests that the horizontal resolution of the GDEM data is around 130 m, somewhat coarser than the sampling interval of 1 second of latitude and longitude. The vertical accuracy is variable, and the factors influencing it have not been systematically explored. However, it appears that the likely accuracy can be estimated from ‘stacking number’ data supplied with the elevation data. The stacking number is the number of independent digital elevation models averaged to generate the supplied product. Provided that this number is greater than around 6 the data have an rms accuracy of typically 5–10 m. Article in Journal/Newspaper Arctic Iceland Polar Record Svalbard Tundra Cambridge University Press Arctic Svalbard Norway Polar Record 48 1 31 39 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development Rees, W. G. Assessment of ASTER global digital elevation model data for Arctic research |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
description |
ABSTRACT A new source of digital elevation data, the advanced spaceborne thermal emission and reflection radiometer (ASTER) global digital elevation model (GDEM), has been freely available since 2009. It provides enormously greater coverage of the Arctic than previous satellite derived ‘global’ digital elevation models, extending to a latitude of 83 °N in contrast to 60 °N. The GDEM is described as a preliminary, research grade product. This paper investigates its accuracy in a number of specifically Arctic landscapes, including ice and snow, boreal forest, tundra and unvegetated terrain, using test sites in Svalbard, Iceland, Norway and Russia. Semivariogram analysis is used to characterise the magnitude and spatial correlation of errors in the GDEM products from the test sites. The analysis suggests that the horizontal resolution of the GDEM data is around 130 m, somewhat coarser than the sampling interval of 1 second of latitude and longitude. The vertical accuracy is variable, and the factors influencing it have not been systematically explored. However, it appears that the likely accuracy can be estimated from ‘stacking number’ data supplied with the elevation data. The stacking number is the number of independent digital elevation models averaged to generate the supplied product. Provided that this number is greater than around 6 the data have an rms accuracy of typically 5–10 m. |
format |
Article in Journal/Newspaper |
author |
Rees, W. G. |
author_facet |
Rees, W. G. |
author_sort |
Rees, W. G. |
title |
Assessment of ASTER global digital elevation model data for Arctic research |
title_short |
Assessment of ASTER global digital elevation model data for Arctic research |
title_full |
Assessment of ASTER global digital elevation model data for Arctic research |
title_fullStr |
Assessment of ASTER global digital elevation model data for Arctic research |
title_full_unstemmed |
Assessment of ASTER global digital elevation model data for Arctic research |
title_sort |
assessment of aster global digital elevation model data for arctic research |
publisher |
Cambridge University Press (CUP) |
publishDate |
2011 |
url |
http://dx.doi.org/10.1017/s0032247411000325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247411000325 |
geographic |
Arctic Svalbard Norway |
geographic_facet |
Arctic Svalbard Norway |
genre |
Arctic Iceland Polar Record Svalbard Tundra |
genre_facet |
Arctic Iceland Polar Record Svalbard Tundra |
op_source |
Polar Record volume 48, issue 1, page 31-39 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247411000325 |
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Polar Record |
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48 |
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1 |
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31 |
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39 |
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