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A Research on Sea Ice Based on Reflected Signals from BeiDou GEO Satellites

机译:基于反射信号的海冰研究了北斗地理卫星的反射信号

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For preventing the effects of sea ice disaster, traditional methods for detecting sea ice have some disadvantages, such as inadequate robustness against weather and high cost of real-time detection. The BeiDou GEO satellites could provide stable geometry and better coverage in mid- and low-latitude region where most of the sea ice occur. Based on this consideration, this paper evaluates the usage of BeiDou GEO Satellites reflected signals for accurate real-time Earth observation to study the changes in the sea surface state through remote sensing. BeiDou GEO signals received after reflection from Bohai Bay were analyzed for their sea ice content. The results are in good agreement with a reflected power ratio model [the ratio of the reflected left-handed circular polarization (LHCP) signals and the reflected right-hand circular polarization (RI ICP) signals] and sea ice concentration. The average of the reflected power ratio on the sea ice surface is much smaller than that on the sea water surface.
机译:为了防止海冰灾害的影响,检测海冰的传统方法具有一些缺点,例如防止天气的鲁棒性和实时检测成本不足。北投地理卫星可以在中低纬度地区提供稳定的几何形状和更好的覆盖范围,其中大部分海冰发生。基于这一考虑,本文评估了北欧地理卫星反射信号的使用,以便通过遥感研究海面状态的变化。分析了渤海湾反射后收到的北投地理信号因其海冰含量。结果与反射功率比率模型(反射左手圆极化(LHCP)信号和反射右手圆极化(RI ICP)信号)和海冰浓度的比率吻合良好。海冰面上反射功率比的平均值远小于海水表面上的电力比。

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