Ocean maybe melting ice shelf from below.Significant portions of a large Antarctic ice shelf just south of one that suddenly broke apart in February 2002 are rapidly thinning and may suffer a similar, catastrophic demise Death. A conveyance of property, usually of an interest in land. Originally meant a posthumous grant but has come to be applied commonly to a conveyance that is made for a definitive term, such as an estate for a term of years. in less than a century, scientists say. Satellite observations collected between 1992 and 2001 suggest that the upper surface of the Larsen C ice shelf dropped as much as 27 centimeters per year during the period. About a quarter of that shrinkage Shrinkage The amount by which inventory on hand is shorter than the amount of inventory recorded. Notes: The missing inventory could be due to theft, damage, or book keeping errors. , or 7 cm, may have resulted from snow packing down into denser material called firn, says Andrew Shepherd, a glaciologist at the University of Cambridge in England. Uncertainties about such factors as the height of ocean tides and the temperature and the salinity sa·line adj. 1. Of, relating to, or containing salt; salty. 2. Of or relating to chemical salts. n. 1. A salt of magnesium or of the alkalis, used in medicine as a cathartic. 2. of water beneath the ice shelf would account for no more than a small fraction of the remaining loss in height above water, says Shepherd. Therefore, he notes, as much as 20 cm per year of the upper surface's drop stems from melting. About nine-tenths of any mass of floating ice lies below the water's surface, suggesting that Larsen C is thinning overall by as much as 2 meters each year. Shepherd and his colleagues report their analysis in the Oct. 31 Science. The likely cause of the thinning, says Shepherd, is relatively warm water beneath the ice shelf. Although water at a depth of 300 m just offshore of the ice shelf's edge is about -1.5[degrees]C, that's about 0.65[degrees]C above the melting point melting point, temperature at which a substance changes its state from solid to liquid. Under standard atmospheric pressure different pure crystalline solids will each melt at a different specific temperature; thus melting point is a characteristic of a substance and for ice at that depth. Many factors, including salinity and pressure, affect ice's melting temperature Melting temperature may refer to:
Even a small temperature increase in the water below an ice shelf can make a big difference in the overlying overlying suffocation of piglets by the sow. The piglets may be weak from illness or malnutrition, the sow may be clumsy or ill, the pen may be inadequate in size or poorly designed so that piglets cannot escape. ice's melting rate, says Eric J. Rignot, a glaciologist at NASA's Jet Propulsion Laboratory “JPL” redirects here. For other uses, see JPL (disambiguation). Jet Propulsion Laboratory (JPL) is a NASA research center located in the cities of Pasadena and La Cañada Flintridge, near Los Angeles, California, USA. in Pasadena, Calif. His research suggests that each O.1[degrees]C rise in water temperature can, in a year's time, melt away about 1 m of shelf ice. In February 2002, 3,250 square kilometers of the Larsen B ice shelf splintered into thousands of icebergs (SN: 3/30/02, p. 197). Shepherd says his team's data suggest that during the previous decade, Larsen B, which was about 200 m thick when it collapsed, was thinning at an average rate of about twice that of Larsen C. Larsen C is stable and isn't shedding more icebergs than normal, says Shepherd. However, at the ice shelf's current rate of thinning, Larsen C could reach a 200-m thickness, and therefore be susceptible to disintegration disintegration /dis·in·te·gra·tion/ (-in?ti-gra´shun) 1. the process of breaking up or decomposing. 2. , in 70 years or so. If the waters in the region continue to warm, the ice shelf's demise could occur even sooner. |
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