Thermal evolution of permeability and microstructure in sea ice

The fluid permeability k of sea ice constrains a broad range of processes, such as the growth and decay of seasonal ice, the evolution of summer ice albedo, and biomass build‐up. Such processes are critical to how sea ice and associated ecosystems respond to climate change. However, studies of k and...

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Veröffentlicht in:	Geophysical research letters 2007-08, Vol.34 (16), p.n/a
Hauptverfasser:	Golden, K. M., Eicken, H., Heaton, A. L., Miner, J., Pringle, D. J., Zhu, J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology microstructure permeability sea ice
Online-Zugang:	Volltext
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