globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-11-363-2017
Scopus记录号: 2-s2.0-85011333397
论文题名:
Generating synthetic fjord bathymetry for coastal Greenland
作者: Williams C; N; , Cornford S; L; , Jordan T; M; , Dowdeswell J; A; , Siegert M; J; , Clark C; D; , Swift D; A; , Sole A; , Fenty I; , Bamber J; L
刊名: Cryosphere
ISSN: 19940416
出版年: 2017
卷: 11, 期:1
起始页码: 363
结束页码: 380
语种: 英语
英文关键词: bathymetry ; fjord ; floating ice ; ice flow ; ice-ocean interaction ; interpolation ; numerical model ; seafloor ; topography ; Arctic ; Australia ; Cape York ; Greenland ; Greenland Ice Sheet ; Queensland
英文摘要: Bed topography is a critical boundary for the numerical modelling of ice sheets and ice-ocean interactions. A persistent issue with existing topography products for the bed of the Greenland Ice Sheet and surrounding sea floor is the poor representation of coastal bathymetry, especially in regions of floating ice and near the grounding line. Sparse data coverage, and the resultant coarse resolution at the ice-ocean boundary, poses issues in our ability to model ice flow advance and retreat from the present position. In addition, as fjord bathymetry is known to exert strong control on ocean circulation and ice-ocean forcing, the lack of bed data leads to an inability to model these processes adequately. Since the release of the last complete Greenland bed topography-bathymetry product, new observational bathymetry data have become available. These data can be used to constrain bathymetry, but many fjords remain completely unsampled and therefore poorly resolved. Here, as part of the development of the next generation of Greenland bed topography products, we present a new method for constraining the bathymetry of fjord systems in regions where data coverage is sparse. For these cases, we generate synthetic fjord geometries using a method conditioned by surveys of terrestrial glacial valleys as well as existing sinuous feature interpolation schemes. Our approach enables the capture of the general bathymetry profile of a fjord in north-west Greenland close to Cape York, when compared to observational data. We validate our synthetic approach by demonstrating reduced overestimation of depths compared to past attempts to constrain fjord bathymetry. We also present an analysis of the spectral characteristics of fjord centrelines using recently acquired bathymetric observations, demonstrating how a stochastic model of fjord bathymetry could be parameterised and used to create different realisations. � Author(s) 2017.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75607
Appears in Collections:影响、适应和脆弱性
气候变化与战略

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作者单位: Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, United Kingdom; Scott Polar Research Institute, University of Cambridge, Cambridge, United Kingdom; Grantham Institute, Department of Earth Science and Engineering, Imperial College London, London, United Kingdom; Department of Geography, University of Sheffield, Sheffield, United Kingdom; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States

Recommended Citation:
Williams C,N,, Cornford S,et al. Generating synthetic fjord bathymetry for coastal Greenland[J]. Cryosphere,2017-01-01,11(1)
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