Articles | Volume 16, issue 1
https://doi.org/10.5194/tc-16-197-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-197-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Towards ice-thickness inversion: an evaluation of global digital elevation models (DEMs) in the glacierized Tibetan Plateau
Wenfeng Chen
CORRESPONDING AUTHOR
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
University of Chinese Academy of Sciences, Beijing, China
Tandong Yao
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Fei Li
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
University of Chinese Academy of Sciences, Beijing, China
Guoxiong Zheng
University of Chinese Academy of Sciences, Beijing, China
Xinjiang Institute of Ecology and Geography, Chinese Academy of
Sciences, Urumqi, China
Yushan Zhou
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Fenglin Xu
State Key Laboratory of Tibetan Plateau Earth System, Resources and
Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
University of Chinese Academy of Sciences, Beijing, China
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Cited
13 citations as recorded by crossref.
- Surface Motion and Topographic Effects on Ice Thickness Inversion for High Mountain Asia Glaciers: A Comparison Study from Three Numerical Models X. Pang et al. 10.3390/rs15225378
- Accuracy assessment of digital bare-earth model using ICESat-2 photons: analysis of the FABDEM G. Dandabathula et al. 10.1007/s40808-022-01648-4
- Ice thickness and morphological analysis reveal the future glacial lake distribution and formation probability in the Tibetan Plateau and its surroundings T. Zhang et al. 10.1016/j.gloplacha.2022.103923
- ICESat-2 river surface slope (IRIS): A global reach-scale water surface slope dataset D. Scherer et al. 10.1038/s41597-023-02215-x
- Glacier mass-balance estimates over High Mountain Asia from 2000 to 2021 based on ICESat-2 and NASADEM Y. Fan et al. 10.1017/jog.2022.78
- Recent Seasonal Spatiotemporal Variations in Alpine Glacier Surface Elevation in the Pamir W. Du et al. 10.3390/rs14194923
- Timing and climatic-driven mechanisms of glacier advances in Bhutanese Himalaya during the Little Ice Age W. Yang et al. 10.5194/tc-16-3739-2022
- Spatial differences of ice volume across High Mountain Asia R. Wang et al. 10.1016/j.accre.2023.08.004
- Late Quaternary lake level record of Orog Nuur, southern Mongolia, revealed by optical dating of paleo-shorelines S. Zhang et al. 10.1016/j.quageo.2022.101370
- Regional “Bare-Earth” Digital Terrain Model for Costa Rica Based on NASADEM Corrected for Vegetation Bias O. Pimenova et al. 10.3390/rs14102421
- Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau L. Gao et al. 10.3390/rs14112634
- Performance assessment of global open‐access digital elevation models in China mainland coastal region H. Ding et al. 10.1002/esp.5677
- Towards ice-thickness inversion: an evaluation of global digital elevation models (DEMs) in the glacierized Tibetan Plateau W. Chen et al. 10.5194/tc-16-197-2022
12 citations as recorded by crossref.
- Surface Motion and Topographic Effects on Ice Thickness Inversion for High Mountain Asia Glaciers: A Comparison Study from Three Numerical Models X. Pang et al. 10.3390/rs15225378
- Accuracy assessment of digital bare-earth model using ICESat-2 photons: analysis of the FABDEM G. Dandabathula et al. 10.1007/s40808-022-01648-4
- Ice thickness and morphological analysis reveal the future glacial lake distribution and formation probability in the Tibetan Plateau and its surroundings T. Zhang et al. 10.1016/j.gloplacha.2022.103923
- ICESat-2 river surface slope (IRIS): A global reach-scale water surface slope dataset D. Scherer et al. 10.1038/s41597-023-02215-x
- Glacier mass-balance estimates over High Mountain Asia from 2000 to 2021 based on ICESat-2 and NASADEM Y. Fan et al. 10.1017/jog.2022.78
- Recent Seasonal Spatiotemporal Variations in Alpine Glacier Surface Elevation in the Pamir W. Du et al. 10.3390/rs14194923
- Timing and climatic-driven mechanisms of glacier advances in Bhutanese Himalaya during the Little Ice Age W. Yang et al. 10.5194/tc-16-3739-2022
- Spatial differences of ice volume across High Mountain Asia R. Wang et al. 10.1016/j.accre.2023.08.004
- Late Quaternary lake level record of Orog Nuur, southern Mongolia, revealed by optical dating of paleo-shorelines S. Zhang et al. 10.1016/j.quageo.2022.101370
- Regional “Bare-Earth” Digital Terrain Model for Costa Rica Based on NASADEM Corrected for Vegetation Bias O. Pimenova et al. 10.3390/rs14102421
- Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau L. Gao et al. 10.3390/rs14112634
- Performance assessment of global open‐access digital elevation models in China mainland coastal region H. Ding et al. 10.1002/esp.5677
Latest update: 27 Nov 2023
Short summary
A digital elevation model (DEM) is a prerequisite for estimating regional glacier thickness. Our study first compared six widely used global DEMs over the glacierized Tibetan Plateau by using ICESat-2 (Ice, Cloud and land Elevation Satellite) laser altimetry data. Our results show that NASADEM had the best accuracy. We conclude that NASADEM would be the best choice for ice-thickness estimation over the Tibetan Plateau through an intercomparison of four ice-thickness inversion models.
A digital elevation model (DEM) is a prerequisite for estimating regional glacier thickness. Our...