Fluid Dynamics and Solid Mechanics Group, Los Alamos National Laboratory, Los Alamos, NM, USA
Viewed
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,785 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,423
296
66
1,785
48
87
HTML: 1,423
PDF: 296
XML: 66
Total: 1,785
BibTeX: 48
EndNote: 87
Views and downloads (calculated since 09 Dec 2024)
Cumulative views and downloads
(calculated since 09 Dec 2024)
Total article views: 1,581 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,225
296
60
1,581
48
87
HTML: 1,225
PDF: 296
XML: 60
Total: 1,581
BibTeX: 48
EndNote: 87
Views and downloads (calculated since 03 Jul 2025)
Cumulative views and downloads
(calculated since 03 Jul 2025)
Total article views: 204 (including HTML, PDF, and XML)
HTML
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Total
BibTeX
EndNote
198
0
6
204
0
0
HTML: 198
PDF: 0
XML: 6
Total: 204
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 09 Dec 2024)
Cumulative views and downloads
(calculated since 09 Dec 2024)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,785 (including HTML, PDF, and XML)
Thereof 1,760 with geography defined
and 25 with unknown origin.
Total article views: 1,581 (including HTML, PDF, and XML)
Thereof 1,555 with geography defined
and 26 with unknown origin.
Total article views: 204 (including HTML, PDF, and XML)
Thereof 204 with geography defined
and 0 with unknown origin.
Subglacial drainage models represent water flow beneath glaciers and ice sheets. Here, we train fast statistical models called Gaussian process (GP) emulators to accelerate subglacial drainage modelling by ~ 1000 times. We use the fast emulator predictions to show that three of the model parameters are responsible for > 90 % of the variance in model outputs. The fast GP emulators will enable future uncertainty quantification and calibration of these models.
Subglacial drainage models represent water flow beneath glaciers and ice sheets. Here, we train...