Modeling VHF Scatter from FY and MY Sea Ice Ridges

P. Bobby, E. Gill, Weimin Huang
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引用次数: 1

Abstract

Declining sea ice conditions are often cited as an indicator of climate change, but limited information is available on sea ice ridges, which comprise up to 50% of ice volume in certain regions. Multi-year (MY) ridges are more hazardous barriers to navigation than first year (FY) ridges and they are more likely to survive the summer melt season, but little effort has been made to identify FY and MY ridges from remote sensing data. This paper describes an analytical method to model electromagnetic scattering from ridges around the VHF range (100–500 MHz) when ridges are modeled as a rough surface over stratified media. Models considering the macroscopic properties of FY and MY ridges relevant to VHF scatter are presented. Simulations show that FY and MY ridges have different scattering characteristics, making it possible to separate the two ice types. Future work will consider how variability in ice ridge characteristics and changes during the ice season affect the separability of FY and MY ridges based on their scattering characteristics.
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FY和MY海冰脊VHF散射模拟
海冰状况的减少通常被认为是气候变化的一个指标,但关于海冰脊的信息有限,在某些地区,海冰脊占冰量的50%。多年脊(MY)是比第一年脊(FY)更危险的导航障碍,它们更有可能在夏季融化季节存活下来,但从遥感数据中识别FY和MY脊的努力很少。本文描述了一种模拟VHF范围(100-500 MHz)附近脊线电磁散射的解析方法,当脊线被模拟为层状介质上的粗糙表面时。提出了考虑了与甚高频散射相关的FY和MY脊的宏观特性的模型。模拟结果表明,FY和MY脊具有不同的散射特性,使两种冰类型的分离成为可能。未来的工作将考虑冰脊特征的变率和冰季变化如何影响FY和MY脊基于其散射特征的可分离性。
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