Ice-wedges in Permafrost, Maranbio Island, Antarctic Peninsula
نویسندگان
چکیده
منابع مشابه
Present stability of the Larsen C ice shelf, Antarctic Peninsula
We modelled the flow of the Larsen C and northernmost Larsen D ice shelves, Antarctic Peninsula, using a model of continuum mechanics of ice flow, and applied a fracture criterion to the simulated velocities to investigate the ice shelf’s present-day stability. Constraints come from satellite data and geophysical measurements from the 2008/09 austral summer. Ice-shelf thickness was derived from...
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متن کاملIce-atmosphere interactions during sea-ice advance and retreat in the western Antarctic Peninsula region
[1] The seasonal evolution of sea-ice extent, concentration, and drift in the western Antarctic Peninsula (WAP) region, along with regional atmospheric synoptic variability, are described for a winter period (1992) when sea-ice advance and retreat were both anomalously early. Daily time series of winds, opening and closing of the sea-ice cover, and volume fluxes in and out of the WAP region ind...
متن کاملAccelerated ice discharge from the Antarctic Peninsula following the collapse of Larsen B ice shelf
[1] Interferometric synthetic-aperture radar data collected by ERS-1/2 and Radarsat-1 satellites show that Antarctic Peninsula glaciers sped up significantly following the collapse of Larsen B ice shelf in 2002. Hektoria, Green and Evans glaciers accelerated eightfold between 2000 and 2003 and decelerated moderately in 2003. Jorum and Crane glaciers accelerated twofold in early 2003 and threefo...
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ژورنال
عنوان ژورنال: Journal of Geography (Chigaku Zasshi)
سال: 1988
ISSN: 0022-135X,1884-0884
DOI: 10.5026/jgeography.97.6_plate1