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Calving rate linearly dependent on sub-aerial terminus cliff height at tidewaters glaciers around the Antarctic Peninsula – ADDENDUM

Part of: Verification and Validation of Cryospheric Models

Published online by Cambridge University Press:  28 August 2025

Richard Parsons Open the ORCID record for Richard Parsons [Opens in a new window] ,
Sainan Sun Open the ORCID record for Sainan Sun [Opens in a new window]  and
Gudmundur Hilmar Gudmundsson Open the ORCID record for Gudmundur Hilmar Gudmundsson [Opens in a new window]
Rights & Permissions [Opens in a new window]

Abstract

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Information

Type
Addendum
Information
Annals of Glaciology , Volume 66 , 2025 , e19
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Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0), which permits unrestricted re- use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2025. Published by Cambridge University Press on behalf of International Glaciological Society.

The authors would like to add the below data availability statement to the originally published article:

Data availability statement

The Reference Elevation Model of Antarctica strip DEMs are openly available from the Polar Geospatial Center Fridge web application and can be accessed at https://fridge.pgc.umn.edu.

Velocity data used in this study from the time period 01 January 2015 to 31 December 2021 are openly available from ENVEO’s CryoPortal, accessible at https://cryoportal.enveo.at/. Velocity data from the time period 01 January 2022 onwards are not currently available due to a reduction in coverage following the failure of Sentinel-1B. Further information may be obtained from https://cryoportal.enveo.at/.

References

Parsons, R, Sun, S and Gudmundsson, GH (2025) Calving rate linearly dependent on sub-aerial terminus cliff height at tidewater claciers around the Antarctic Peninsula. Annals of Glaciology 66, e13. https://doi.org/10.1017/aog.2025.10008CrossRefGoogle Scholar