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Polar Research Volume 35, 2016 - Issue 1
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Research/review articles

Relation between planimetric and volumetric measurements of permafrost coast erosion: a case study from Herschel Island, western Canadian Arctic

Jaroslav ObuDepartment of Periglacial ResearchAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, DE-14473 Potsdam, Germany;Institute of Earth and Environmental ScienceUniversity of Potsdam, Am Neuen Palais 10, DE-14469 Potsdam, Germany;Department of GeosciencesUniversity of Oslo, PO Box 1047, NO-0316 Blindern, Oslo, NorwayCorrespondence[email protected]
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Hugues LantuitDepartment of Periglacial ResearchAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, DE-14473 Potsdam, Germany;Institute of Earth and Environmental ScienceUniversity of Potsdam, Am Neuen Palais 10, DE-14469 Potsdam, Germany
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Michael FritzDepartment of Periglacial ResearchAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, DE-14473 Potsdam, Germany;Department of Earth SciencesUtrecht University, Heidelberglaan 2, NL-3584CS Utrecht, The Netherlands
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Wayne H. PollardDepartment of GeographyMcGill University, 805Sherbrooke Street West, Montreal, Canada
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Torsten SachsGerman Research Centre for Geosciences, Telegrafenberg, DE-14473Potsdam, Germany
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Frank GüntherDepartment of Periglacial ResearchAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Telegrafenberg A43, DE-14473 Potsdam, Germany
Article: 30313 | Published online: 23 Sep 2016

Related Research Data

Long-Term High-Resolution Sediment and Sea Surface Temperature Spatial Patterns in Arctic Nearshore Waters Retrieved Using 30-Year Landsat Archive Imagery
Source: HAL CCSD
Dynamics of Permafrost Coasts of Baydaratskaya Bay (Kara Sea) Based on Multi-Temporal Remote Sensing Data
Source: MDPI AG
Burial and Origin of Permafrost-Derived Carbon in the Nearshore Zone of the Southern Canadian Beaufort Sea
Source: FID GEO
Remote sensing evaluation of High Arctic wetland depletion following permafrost disturbance by thermo-erosion gullying processes1
Source: Canadian Science Publishing

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