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Ocean-forcing and glacier-specific factors drive differing glacier response across the 69 N boundary, east Greenland.

Lookup NU author(s): Dr Stephen Brough, Professor Rachel CarrORCiD, Professor Neil RossORCiD

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This work is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0).

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Author(s): Brough S, Carr JR, Ross N, Lea J

Publication type: Article

Publication status: Published

Journal: Journal of Geophysical Research

Year: 2023

Volume: 128

Issue: 4

Print publication date: 01/04/2023

Online publication date: 02/03/2023

Acceptance date: 21/02/2023

Date deposited: 24/02/2023

ISSN (print): 2169-9003

ISSN (electronic): 2169-9011

Publisher: Wiley-Blackwell Publishing, Inc.

URL: https://doi.org/10.1029/2022JF006857

DOI: 10.1029/2022JF006857

Data Access Statement: Terminus data generated in this study are archived for download via Brough (2023), https://doi.org/10.5281/zenodo.6904219. We also used a number of openly available datasets used in this study (also summarized in Table S1 in Supporting Information S1). Ice velocity maps of Scambos et al. (2016) can be accessed from https://doi.org/10.7265/N5ZP442B; Joughin (2020) can be accessed from https://doi.org/10.5067/11MJZGPBK3ZF; Joughin et al. (2020) can be accessed from https://doi.org/10.5067/YXMJRME5OUNC; and Solgaard and Kusk (2021) can be accessed from https://doi.org/10.22008/promice/data/sentinel1icevelocity/greenlandicesheet. Surface air temperature data of Cappelen (2021) can be accessed from https://www.dmi.dk/publikationer/ [see article for full data access statement].

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