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Sökning: WFRF:(Dowdeswell Julian A.) > (2015-2019) > Application of a tw...

Application of a two-step approach for mapping ice thickness to various glacier types on Svalbard

Fuerst, Johannes Jakob (författare)
University of Erlangen-Nuremberg, Institute of Geography
Gillet-Chaulet, Fabien (författare)
University of Grenoble Alpes, CNRS, IRD, Institut des Géosciences de l’Environnement (IGE)
Benham, Toby J. (författare)
University of Cambridge, Scott Polar Research Institute
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Dowdeswell, Julian A. (författare)
University of Cambridge, Scott Polar Research Institute
Grabiec, Mariusz (författare)
University of Silesia in Katowice, Faculty of Earth Sciences
Navarro, Francisco (författare)
Universidad Politécnica de Madrid, Departamento de Matemática Aplicada a las Tecnologías de la Información y las Comunicaciones, desp. A302-4, ETSI de Telecomunicación
Pettersson, Rickard (författare)
Uppsala universitet,Luft-, vatten- och landskapslära
Moholdt, Geir (författare)
Norwegian Polar Institute, Fram Centre
Nuth, Christopher (författare)
University of Oslo, Department of Geoscience
Sass, Björn (författare)
University of Erlangen-Nuremberg, Institute of Geography
Aas, Kjetil (författare)
University of Oslo, Department of Geoscience
Fettweis, Xavier (författare)
University of Liège, Department of Geography
Lang, Charlotte (författare)
University of Liège, Department of Geography
Seehaus, Thorsten (författare)
University of Erlangen-Nuremberg, Institute of Geography
Braun, Matthias (författare)
University of Erlangen-Nuremberg, Institute of Geography
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 (creator_code:org_t)
2017-09-01
2017
Engelska.
Ingår i: The Cryosphere. - : Copernicus GmbH. - 1994-0416 .- 1994-0424. ; 11:5, s. 2003-2032
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The basal topography is largely unknown beneath most glaciers and ice caps, and many attempts have been made to estimate a thickness field from other more accessible information at the surface. Here, we present a two-step reconstruction approach for ice thickness that solves mass conservation over single or several connected drainage basins. The approach is applied to a variety of test geometries with abundant thickness measurements including marine-and landterminating glaciers as well as a 2400 km(2) ice cap on Svalbard. The input requirements are kept to a minimum for the first step. In this step, a geometrically controlled, non-local flux solution is converted into thickness values relying on the shallow ice approximation (SIA). In a second step, the thickness field is updated along fast-flowing glacier trunks on the basis of velocity observations. Both steps account for available thickness measurements. Each thickness field is presented together with an error-estimate map based on a formal propagation of input uncertainties. These error estimates point out that the thickness field is least constrained near ice divides or in other stagnant areas. Withholding a share of the thickness measurements, error estimates tend to overestimate mismatch values in a median sense. We also have to accept an aggregate uncertainty of at least 25% in the reconstructed thickness field for glaciers with very sparse or no observations. For Vestfonna ice cap (VIC), a previous ice volume estimate based on the same measurement record as used here has to be corrected upward by 22 %. We also find that a 13% area fraction of the ice cap is in fact grounded below sea level. The former 5% estimate from a direct measurement interpolation exceeds an aggregate maximum range of 6-23% as inferred from the error estimates here.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

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