Frontiers in Digital Humanities | |
Unraveling InSAR Observed Antarctic Ice-Shelf Flexure Using 2-D Elastic and Viscoelastic Modeling | |
Marsh, Oliver J.1  Wild, Christian T.1  Rack, Wolfgang1  | |
[1] Gateway Antarctica, University of Canterbury, New Zealand | |
关键词: Synthetic aperture radar (SAR); Differential SAR interferometry (DInSAR); numerical modelling; TerraSAR-X; Cryosat-2; Antarctica; Ice shelf; grounding line; | |
DOI : 10.3389/feart.2018.00028 | |
学科分类:社会科学、人文和艺术(综合) | |
来源: Frontiers | |
【 摘 要 】
Ice-shelf grounding zones link the Antarctic ice-sheets to the ocean. Differential interferometric synthetic aperture radar (DInSAR) is commonly used to monitor grounding-line locations, but also contains information on grounding-zone ice thickness, ice properties and tidal conditions beneath the ice shelf. Here, we combine in-situ data with numerical modelling of ice-shelf flexure to investigate 2-D controls on the tidal bending pattern on the Southern McMurdo Ice Shelf. We validate our results with 9 double-differential TerraSAR-X interferograms. It is necessary to make adjustments to the tidal forcing to directly compare observations with model output and we find that when these adjustments are small (< 1.5 cm) a viscoelastic model matches better, while an elastic model is more robust overall. Within landward embayments, where lateral stresses from surrounding protrusions damp the flexural response, a 2-D model captures behaviour that is missed in simple 1-D models. We conclude that improvements in current tide models are required to allow for the full exploitation of DInSAR in grounding-zone glaciology.
【 授权许可】
CC BY
【 预 览 】
Files | Size | Format | View |
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RO201904024648454ZK.pdf | 3230KB | download |