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Noel Gourmelen

Researcher at University of Edinburgh

Publications -  104
Citations -  3358

Noel Gourmelen is an academic researcher from University of Edinburgh. The author has contributed to research in topics: Glacier & Ice sheet. The author has an hindex of 28, co-authored 93 publications receiving 2503 citations. Previous affiliations of Noel Gourmelen include University of Miami & University of Leeds.

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Decadal slowdown of a land-terminating sector of the Greenland Ice Sheet despite warming

TL;DR: It is shown that annual ice motion across an 8,000-km2 land-terminating region of the west GIS margin, extending to 1,100 m above sea level, was 12% slower in 2007–14 compared with 1985–94, despite a 50% increase in surface meltwater production.
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Mining-related ground deformation in Crescent Valley, Nevada: Implications for sparse GPS networks

TL;DR: In this paper, the Small BAseline Subset (SBAS) algorithm was used to obtain radar line-of-sight deformation velocities for two adjacent SAR swaths and invert the data for the 2-D velocity field in vertical and ground range direction.
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InSAR observations of 2007 Tanzania rifting episode reveal mixed fault and dyke extension in an immature continental rift

TL;DR: In the early stages of continental rifting, extension takes place by normal faulting, while in mature continental rifts dyke intrusion dominates as discussed by the authors, which is known about the nature of the transition between fault-controlled and dyke-controlled extension.
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Postseismic Mantle Relaxation in the Central Nevada Seismic Belt

TL;DR: Interferometric synthetic aperture radar detected a broad area of uplift that can be explained by postseismic mantle relaxation after a sequence of large crustal earthquakes from 1915 to 1954 and lead to a broad agreement between geologic and geodetic strain indicators.
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Sustained retreat of the Pine Island Glacier

TL;DR: In this paper, the authors used satellite observations to show that, between 1992 and 2011, the Pine Island Glacier hinge line retreated at a rate of 0.95 ± 0.09 km yr−1 despite a progressive steepening and shoaling of the glacier surface and bedrock slopes, respectively.