標(biāo)題: Titlebook: Drift, Deformation, and Fracture of Sea Ice; A Perspective Across Jér?me Weiss Book 2013 The Author(s) 2013 Arctic Sea Ice.Evolution of Sea [打印本頁] 作者: Pessimistic 時間: 2025-3-21 18:52
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作者: Indebted 時間: 2025-3-21 23:12 作者: 譏諷 時間: 2025-3-22 01:29
Sea Ice Fracturing,tion patterns as seen in aerial or satellite images on the other hand. In-situ stress records show that sea ice internal stress states lie within a Coulombic envelope whose shape and the associated internal friction coefficient are very similar to that obtained from brittle compressive failure tests作者: anachronistic 時間: 2025-3-22 07:20
Conclusion and Perspectives: Sea Ice Drift, Deformation and Fracturing in a Changing Arctic,e last decades. For more than 30?years now, increasing average drift velocities and deformation rates, in both summer and winter, not only accompanied but most likely strengthened the Arctic sea ice decline through a modification of the albedo feedback. Indeed, a thinner ice cover means more fractur作者: 墻壁 時間: 2025-3-22 09:19 作者: heterogeneous 時間: 2025-3-22 14:32 作者: heterogeneous 時間: 2025-3-22 18:46
Jér?me WeissIncludes supplementary material: 作者: CERE 時間: 2025-3-22 23:55 作者: hemophilia 時間: 2025-3-23 04:21
Lecture Notes in Computer ScienceIn this introductory chapter, after a short historical perspective on sea ice drift studies from the pioneering observations of Nansen, we briefly introduce the momentum equation of sea ice as well as some generic definitions, tools and concepts that will be used afterwards in this book to analyze the scaling properties of the sea ice cover.作者: 動脈 時間: 2025-3-23 08:26
Introduction,In this introductory chapter, after a short historical perspective on sea ice drift studies from the pioneering observations of Nansen, we briefly introduce the momentum equation of sea ice as well as some generic definitions, tools and concepts that will be used afterwards in this book to analyze the scaling properties of the sea ice cover.作者: Coterminous 時間: 2025-3-23 11:26 作者: Incumbent 時間: 2025-3-23 14:41
Vasculitis in Clinical Practiceanalysis of the relative dispersion of tracers (buoys), or from strain-rate fields obtained from satellite imagery. Although statistical tools previously developed in the context of turbulence have been used to characterize sea ice dispersion, the differences between sea ice and turbulent fluids are作者: 策略 時間: 2025-3-23 18:53 作者: 紋章 時間: 2025-3-23 23:40 作者: 半導(dǎo)體 時間: 2025-3-24 03:05
2191-5369 les. Indeed, owing to its very strong kinematics, compared e.g. to the Earth’s crust, an unrivaled kinematical data set is available for sea ice from in situ (e.g. drifting buoys) or satellite 978-94-007-6201-5978-94-007-6202-2Series ISSN 2191-5369 Series E-ISSN 2191-5377 作者: WATER 時間: 2025-3-24 09:49 作者: JUST 時間: 2025-3-24 13:08 作者: 謙卑 時間: 2025-3-24 15:16 作者: accrete 時間: 2025-3-24 22:47
Sea Ice Deformation, slightly super-diffusive regime at small spatial scales, to a very slow sub-diffusive one at large scales, i.e. much slower than oceanic dispersion. This also argues for a strongly non-linear, brittle rheology of the sea ice cover.作者: Adherent 時間: 2025-3-25 02:35 作者: nascent 時間: 2025-3-25 05:45 作者: GAVEL 時間: 2025-3-25 09:51 作者: 發(fā)微光 時間: 2025-3-25 14:11
Video Analytics for Audience Measurementotion, or intermittency. However, significant differences are also observed: sea ice velocity distributions are clearly much more spread than Gaussian statistics, intermittency is more pronounced, and sea ice accelerations cannot be explained from wind stress statistics. These differences argue for a non-linear response of sea ice to forcing.作者: 放逐 時間: 2025-3-25 17:26 作者: 中世紀(jì) 時間: 2025-3-25 22:34
Andreas Kleefeld,Bernhard Burgethcover has been highlighted from a strengthening of inertial oscillations. This interweaving of the sea ice state (thickness, concentration) in the one hand, and mechanical/dynamical processes on the other hand, calls for a continuing effort on the analysis of sea ice drift, deformation and fracturing.作者: wreathe 時間: 2025-3-26 01:47 作者: 粗語 時間: 2025-3-26 04:51
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