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Arctic sea ice

2016
The Arctic sea ice has been in decline during the last three decades, and the Arctic summer sea ice extent has never been as low as at present during the last 1450 years. Natural variability alone cannot explain the recent observed decrease. There is a direct physical argument that climate change causes a decrease of sea ice: an increase of atmospheric
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An Ice Free Arctic Sea? The Science of Sea Ice and Its Interests

2013
The 2007 sea-ice minimum was quickly framed as a unique event and a very clear signal that the Arctic was a bellwether for global climate change. It became an event of the future it heralded rather than of the past or recent changes that had created it.
Sverker Sörlin, Julia Lajus
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Sea ice deformation and sea ice thickness change

2022
The Arctic Ocean is undergoing a major transition from a year-round sea ice cover to ice-free summers with global consequences. Sea ice thickness is at the center of the ongoing changes because the thickness regulates key processes of the Arctic climate system and in the last six decades, the mean thickness has more than halved.
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Perscribing Antarctic landfast sea ice in a sea ice-ocean model.

The coastal polynyas of the Southern Ocean play a crucial role in the formation of dense water and have an impact on the stability of ice shelves. Therefore, it is important to accurately simulate them in climate models. To achieve this goal, the relationship between grounded icebergs, landfast ice and polynyas appears to be central.
Noé Pirlet   +7 more
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Sea Ice

2015
The second edition of Sea Ice: Physics and Remote Sensing has been revised and updated to reflect the latest developments in geophysical sensors and ice parameters retrieval techniques. This volume addresses experiences acquired mainly in Canada by researchers in the fields of ice physics and growth history in relation to its polycrystalline structure ...
Shokr, Mohammed, Sinha, Nirmal K.
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Sea Ice Mechanics Research

1997
Abstract : The ultimate goal of our research is the development of a complete ice dynamics model that will include ice stress, lead direction, and ice thickness distribution in refrozen leads.
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Sea Ice Drift

2013
In this chapter, sea ice drift is discussed in terms of statistical properties of individual Lagrangian trajectories. It is first shown that the Arctic sea ice velocity field can be objectively decomposed into a mean field and fluctuations. The mean field shows intra-annual (between winter and summer) as well as some interannual variability.
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Sea Ice

Geographical Review, 1938
Floyd M. Soule, Josef Zukriegel
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