Temporal and spatial changes of the basal channel of the Getz Ice Shelf in Antarctica derived from multi-source data
Author:
Publisher
Springer Science and Business Media LLC
Subject
Aquatic Science,Oceanography
Link
https://link.springer.com/content/pdf/10.1007/s13131-022-1989-1.pdf
Reference65 articles.
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2. Arneborg L, Wåhlin A K, Björk G, et al. 2012. Persistent inflow of warm water onto the central Amundsen shelf. Nature Geoscience, 5(12): 876–880, doi: https://doi.org/10.1038/ngeo1644
3. Assmann K M, Darelius E, Wåhlin A K, et al. 2019. Warm circumpolar deep water at the western Getz Ice Shelf front, Antarctica. Geophysical Research Letters, 46(2): 870–878, doi: https://doi.org/10.1029/2018GL081354
4. Bindschadler R, Vaughan D G, Vornberger P. 2011. Variability of basal melt beneath the Pine Island Glacier ice shelf, West Antarctica. Journal of Glaciology, 57(204): 581–595, doi: https://doi.org/10.3189/002214311797409802
5. Borsa A A, Moholdt G, Fricker H A, et al. 2014. A range correction for ICESat and its potential impact on ice-sheet mass balance studies. The Cryosphere, 8(2): 345–357, doi: https://doi.org/10.5194/tc-8-345-2014
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