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Radar backscatter measurements from Arctic sea ice during the fall freeze-up

机译:秋季冻结期间北极海冰的雷达反向散射测量

摘要

Radar backscatter measurements from sea ice during the fall freeze-up were performed by the United States Coast Guard Icebreaker Polar Star as a part of the International Arctic Ocean Expedition (IAOE'91) from Aug. to Sep. 1991. The U.S. portion of the experiment took place on board the Polar Star and was referred to as TRAPOLEX '91 (Transpolar expedition) by some investigators. Before prematurely aborting its mission because of mechanical failure of her port shaft, the Polar Star reached 84 deg 57 min N latitude at 35 deg E longitude. The ship was in the ice (greater than 50 percent coverage) from 14 Aug. until 3 Sep. and was operational for all but 6 days due to two instances of mechanical problems with the port shaft. The second was fatal to the ship's participation in the expedition. During the expedition, radar backscatter was measured at C-band under a variety of conditions. These included measurements from young ice types as well as from multiyear and first-/second-year sea ice during the fall freeze-up. The sea ice types were determined by measurement of the ice properties at several of the stations and by visual inspection on others. Radar backscatter measurements were performed over a large portion of the ship's transit into the Arctic ice pack. These were accompanied by in situ sea ice property characterization by the U.S. Army Cold Regions Research and Engineering Laboratory (CRREL) at several stations and, when snow was present, its properties were documented by The Microwave Group, Ottawa River (MWG).
机译:1991年8月至9月间,作为国际北冰洋探险队(IAOE'91)的一部分,美国海岸警卫队破冰船极地星号进行了秋季冰冻期间海冰的雷达反向散射测量。实验是在北极星号上进行的,一些研究人员将其称为TRAPOLEX '91(跨极探险)。由于她的左舷轴机械故障而提前中止其任务之前,“北极星”在东经35度达到北纬84度57分。从8月14日至9月3日,该船处于冰层中(覆盖率超过50%),由于两次发生井口竖井机械故障,该船在除6天外的所有时间内均能运转。第二个对舰队参加这次探险是致命的。在考察期间,在各种条件下在C波段测量了雷达的反向散射。这些测量包括来自年轻冰类型以及秋季冻结期间多年和第一/第二年海冰的测量。海冰类型是通过测量几个站点的冰属性并通过目视检查其他站点来确定的。雷达向后散射测量是在船舶大部分进入北极冰袋的过程中进行的。这些伴随着美国陆军寒冷地区研究与工程实验室(CRREL)在几个站点进行的原位海冰特性表征,当有雪出现时,其特性由渥太华河微波集团(MWG)记录。

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