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Eric Kendrick

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Recent Articles
1.
Gomez D, Bevis M, Smalley Jr R, Durand M, Willis M, Caccamise 2nd D, et al.
Sci Rep . 2022 Jun; 12(1):9553. PMID: 35688878
The Patagonia Icefields (PIF) are the largest non-polar ice mass in the southern hemisphere. The icefields cover an area of approximately 16,500 km and are divided into the northern and...
2.
Weiss J, Qiu Q, Barbot S, Wright T, Foster J, Saunders A, et al.
Sci Adv . 2020 Feb; 5(12):eaax6720. PMID: 32064315
Deformation associated with plate convergence at subduction zones is accommodated by a complex system involving fault slip and viscoelastic flow. These processes have proven difficult to disentangle. The 2010 8.8...
3.
Bevis M, Harig C, Khan S, Brown A, Simons F, Willis M, et al.
Proc Natl Acad Sci U S A . 2019 Jan; 116(6):1934-1939. PMID: 30670639
From early 2003 to mid-2013, the total mass of ice in Greenland declined at a progressively increasing rate. In mid-2013, an abrupt reversal occurred, and very little net ice loss...
4.
Barletta V, Bevis M, Smith B, Wilson T, Brown A, Bordoni A, et al.
Science . 2018 Jun; 360(6395):1335-1339. PMID: 29930133
The marine portion of the West Antarctic Ice Sheet (WAIS) in the Amundsen Sea Embayment (ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is vulnerable...
5.
Bevis M, Wahr J, Khan S, Madsen F, Brown A, Willis M, et al.
Proc Natl Acad Sci U S A . 2012 Jul; 109(30):11944-8. PMID: 22786931
The Greenland GPS Network (GNET) uses the Global Positioning System (GPS) to measure the displacement of bedrock exposed near the margins of the Greenland ice sheet. The entire network is...