Drift, Deformation, and Fracture of Sea Ice : A Perspective Across Scales


Jerome. Weiss
Bok Engelsk 2013 · Electronic books.
Annen tittel
Medvirkende
Thorndike, A. S (Editor)
Utgitt
Springer , 2013
Omfang
1 online resource (83 p.)
Opplysninger
Description based upon print version of record.. - ""Drift, Deformation, and Fracture of Sea Ice""; ""Foreword""; ""Further Readings""; ""Contents""; ""Symbols""; ""1 Introduction""; ""Abstract""; ""1.1�Sea Ice Kinematics: From the Fram�s Journey to Thorndike�s Legacy""; ""1.2�The Momentum Equation of Sea Ice""; ""1.3�Scaling: Some Basic Definitions""; ""References""; ""2 Sea Ice Drift""; ""Abstract""; ""2.1�Data""; ""2.2�How to Extract a Mean Field""; ""2.3�Diffusion Regimes""; ""2.4�Turbulent-Like Fluctuations""; ""2.5�Sea Ice Acceleration and the Dynamical Origin of Intermittency""; ""2.6�Spectral Analysis"". - ""2.7�Concluding Remarks""""References""; ""3 Sea Ice Deformation""; ""Abstract""; ""3.1�Data""; ""3.2�Spatial Scaling and Localization of Deformation""; ""3.3�Spatial and Temporal Scaling Laws from the Dispersion of Lagrangian Trajectories""; ""3.4�Space/Time Coupling""; ""3.5�Sea Ice Dispersion as the Result of ��Solid Turbulence��""; ""3.6�Spectral Analysis""; ""3.7�Concluding Remarks""; ""References""; ""4 Sea Ice Fracturing""; ""Abstract""; ""4.1�Data""; ""4.2�Sea Ice Internal Stresses, Strength, and Rheology""; ""4.3�Intermittency of Sea Ice Stresses"". - ""4.4�Fracture Networks""""4.5�A Statistical Model of Sea Ice Fracturing and Deformation""; ""5 Conclusion and Perspectives: Sea Ice Drift, Deformation and Fracturing in a Changing Arctic""; ""Abstract""; ""References"". - 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 i
Emner
Glaciers.
Sea ice drift.
Sea ice.
Snow.
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Dewey
ISBN
9789400762015

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