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ICE THICKNESS ESTIMATION METHOD BY SAR

机译:SAR测冰厚度的方法

摘要

PPROBLEM TO BE SOLVED: To provide a method for determining the ice thickness accurately from a back scattering coefficient by clarifying a mechanism of back scattering by paying attention to a characteristic of the sea ice having salinity or bubbles. PSOLUTION: In this method for estimating the ice thickness by remote sensing by a SAR, if the back scattering coefficient is smaller mainly because of surface scattering, proportionally at a portion having the larger thickness of the object ice, the object ice is determined to be first-year ice, and if the back scattering coefficient is larger mainly because of volume scattering, proportionally at a portion having the smaller thickness of the object ice, the object ice is determined to be many-year ice. Classification between the first-year ice and the many-year ice may be performed by setting a threshold of the back scattering coefficient at 10 dB. PCOPYRIGHT: (C)2006,JPO&NCIPI
机译:<要解决的问题:提供一种方法,该方法通过通过关注具有盐度或气泡的海冰的特征来阐明反向散射的机理,从而通过反向散射系数来精确地确定冰厚。

解决方案:在这种通过SAR遥感估算冰厚度的方法中,如果主要由于表面散射而导致后向散射系数较小,则在目标冰厚度较大的部分按比例分配目标冰是如果将后向散射系数确定为第一年冰,并且如果主要由于体积散射而使后向散射系数较大,则在对象冰的厚度较小的部分成比例地确定该目标冰为多年冰。第一年冰和多年冰之间的分类可以通过将反向散射系数的阈值设置为10 dB来执行。

版权:(C)2006,JPO&NCIPI

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