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SEA ICE PROPERTIES ON THE USCGC HEALY ICE TRIALS

机译:USCGC热冰试验的海冰特性

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摘要

During the USCGC Healy ice trials in Baffin Bay in April/May 2000, the sea ice thickness and strength, as well as the snow thickness, were measured. The thickness of the ice was measured by augering, by an electromagnetic (EM) method, from cores, and with an Over-The-Side-Video (OTSV). Good agreement was found from these methods in the first year ice, but less good for the two cores of multi-year ice. The snow thickness was measured by point survey measurements and from the OTSV. The OTSV method gave snow thicknesses consistently greater than the point measurements. These different methods are described and the results obtained are discussed. Sea ice strength was determined by drilling cores either by hand or with the RapidCore equipment, measuring temperature, salinity and density, and then calculating flexural strength. The mean strength of the first year ice was 315 kPa (46 psi) and the mean strength of two multi-year cores was 714 kPa (104 psi).
机译:在2000年4月/ 5月在巴芬湾(Baffin Bay)进行的USCGC Healy冰试验期间,测量了海冰厚度和强度以及积雪厚度。冰的厚度是通过电磁波(EM)方法从岩心上进行浮雕测量,并使用超视像(OTSV)测量的。这些方法在第一年的冰中发现了很好的一致性,但是对于多年冰的两个核心而言却没有那么好。积雪厚度是通过点调查测量和OTSV测量的。 OTSV方法给出的积雪厚度始终大于点测量值。描述了这些不同的方法,并讨论了获得的结果。通过手动或使用RapidCore设备钻芯来确定海冰强度,测量温度,盐度和密度,然后计算抗弯强度。第一年冰的平均强度为315 kPa(46 psi),两个多年核心的平均强度为714 kPa(104 psi)。

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