物理、电气和微波的检验,海水演变成年轻的冰

R. Onstott
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引用次数: 3

摘要

摘要:了解海冰厚度、温度分布、盐度分布、介电特性分布和空气-冰界面粗糙度之间的相互关系,对于理解新生海冰和新生海冰的后向散射响应具有重要意义。在实验室室外槽中生长的盐水冰盖生长的前120小时内,对其进行了后向散射、物理和电学特性测量。这项工作的目的是描述开放水域到15厘米厚冰的演变过程。环境空气温度为-15℃,在生长到10厘米的关键时期,然后在生长的最后5厘米时加热到10℃。利用5.3、9.6、13.6和16.6 GHz波段的雷达后向散射数据,分析了冰厚、冰表面温度、盐度剖面、介电剖面以及冰-气界面自然变化对微波特征的影响。采用线性天线发射-接收极化,包括垂直-垂直极化和水平-水平极化。入射角扫描从垂直到50度。记录并讨论了随冰厚度变化的后向散射响应的变化,并根据物理-化学-电学性质的变化进行了讨论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Examination of the Physical, Electrical, and Microwave, Evolution of Sea Water Into Young Ice
Abstract : Knowledge of the interrelationships between ice thickness, its temperature profile, the distribution of salinity, the dielectric property profile, and the roughness of the air-ice interface is important to the understanding of the backscatter response of new and young sea ice. Backscatter, physical, and electrical property measurements were made during the first 120 hours of growth for a saline ice sheet grown in a laboratory outdoor tank. The purpose of this work is to describe the evolution of open water to ice 15 cm thick. Ambient air temperatures were -15 deg C. During the critical growth period to 10 cm and then warmed to 10 deg C during the final 5 cm of growth. Radar backscatter data were obtained at 5.3, 9.6, 13.6, and 16.6 GHz to correlate with the changes in the microwave signatures with ice thickness, ice surface temperature, the salinity profile, the dielectric profile, and modifications which occur naturally to the air-ice interface of the ice sheet. Linear antenna transmit-receive polarizations were used and include vertical- vertical and horizontal-horizontal. Angle of incidence scans were made from vertical to 50 deg. The change in the backscatter response with changing ice thickness is documented and discussed in terms of the physical-chemical- electrical property changes.
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