| Autor: |
Golden KM; K. M. Golden, Department of Mathematics, University of Utah, Salt Lake City, UT 84112, USA. S. F. Ackley, U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, NH 03755, USA. V. I. Lytle, Antarctic Cooperative Research Centre a., Ackley SF, Lytle VI VI |
| Jazyk: |
angličtina |
| Zdroj: |
Science (New York, N.Y.) [Science] 1998 Dec 18; Vol. 282 (5397), pp. 2238-41. |
| DOI: |
10.1126/science.282.5397.2238 |
| Abstrakt: |
Sea ice exhibits a marked transition in its fluid transport properties at a critical brine volume fraction pc of about 5 percent, or temperature Tc of about -5 degreesC for salinity of 5 parts per thousand. For temperatures warmer than Tc, brine carrying heat and nutrients can move through the ice, whereas for colder temperatures the ice is impermeable. This transition plays a key role in the geophysics, biology, and remote sensing of sea ice. Percolation theory can be used to understand this critical behavior of transport in sea ice. The similarity of sea ice microstructure to compressed powders is used to theoretically predict pc of about 5 percent. |
| Databáze: |
MEDLINE |
| Externí odkaz: |
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