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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

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發(fā)表于 2025-3-21 18:52:59 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Drift, Deformation, and Fracture of Sea Ice
副標(biāo)題A Perspective Across
編輯Jér?me Weiss
視頻videohttp://file.papertrans.cn/283/282859/282859.mp4
概述Includes supplementary material:
叢書名稱SpringerBriefs in Earth Sciences
圖書封面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
描述.Sea ice is a major component of polar environments, especially in the Arctic where it covers the entire Arctic Ocean throughout most of the year. However, in the context of climate change, the Arctic sea ice cover has been declining significantly over the last decades, either in terms of its concentration or thickness. The sea ice cover evolution and climate change are strongly coupled through the albedo positive feedback, thus possibly explaining the Arctic amplification of climate warming. In addition to thermodynamics, sea ice kinematics (drift, deformation) appears as an essential factor in the evolution of the ice cover through a reduction of the average ice age (and consequently of the cover‘s thickness), or ice export out of the Arctic. This is a first motivation for a better understanding of the kinematical and mechanical processes of sea ice. A more upstream, theoretical motivation is a better understanding of the brittle deformation of geophysical objects across a wide range of scales. 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
出版日期Book 2013
關(guān)鍵詞Arctic Sea Ice; Evolution of Sea Ice; Modeling of Sea Ice; Sea Ice Deformation; Sea Ice Drift; Sea Ice Ki
版次1
doihttps://doi.org/10.1007/978-94-007-6202-2
isbn_softcover978-94-007-6201-5
isbn_ebook978-94-007-6202-2Series ISSN 2191-5369 Series E-ISSN 2191-5377
issn_series 2191-5369
copyrightThe Author(s) 2013
The information of publication is updating

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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
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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
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Jér?me WeissIncludes supplementary material:
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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.
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發(fā)表于 2025-3-23 08:26:57 | 只看該作者
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.
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