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James R. Jordan

Researcher at Northumbria University

Publications -  18
Citations -  451

James R. Jordan is an academic researcher from Northumbria University. The author has contributed to research in topics: Ice shelf & Glacier. The author has an hindex of 9, co-authored 13 publications receiving 311 citations. Previous affiliations of James R. Jordan include British Antarctic Survey & Bangor University.

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Impact of tidal energy converter (TEC) arrays on the dynamics of headland sand banks

TL;DR: In this article, the authors investigate the impact of TEC array operation on headland sand bank formation, followed by a case study, the Alderney Race, in the Channel Islands and Cap de la Hague (France).
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Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2)

Anders Levermann, +46 more
TL;DR: In this article, the authors apply a linear response theory approach to 16 state-of-the-art ice sheet models to estimate the Antarctic ice sheet contribution from basal ice shelf melting within the 21st century.
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Intermittent structural weakening and acceleration of the Thwaites Glacier Tongue between 2000 and 2018.

TL;DR: In this paper, the authors used remote sensing observations to investigate recent changes in the structure and velocity of Thwaites Glacier and its floating tongue, and found that the main trunk of the glacier has accelerated by 38% over this period, while its previously intact floating tongue has transitioned to a weaker melange of fractured icebergs bounded by sea ice.
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Ocean-forced ice-shelf thinning in a synchronously coupled ice-ocean model

TL;DR: In this article, the first fully synchronous, coupled ice shelf-ocean model with a fixed grounding line and imposed upstream ice velocity has been developed using the MITgcm (Massachusetts Institute of Technology general circulation model).
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The Response of Ice Sheets to Climate Variability

TL;DR: In this article, the response of an ice sheet to periodic variations in ocean forcing is evaluated using a synchronously coupled ice-ocean model permitting grounding line migration, and the results highlight the sensitivity of West Antarctic ice streams to perturbations in heat fluxes occurring at decadal time scales.