基于神经网络的卫星无源微波冰浓度反演算法

L. Bobylev, E. Zabolotskikh, L. Mitnik, O. Johannessenn
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引用次数: 2

摘要

考虑到多年冰是北极气候变化的关键指标之一,现有的多年冰覆盖观测算法在多年分数计算中不准确,这是现有全球冰监测系统的一个显著缺陷。本文采用数值实验的封闭格式,提出了基于区域差分神经网络(NN)的北极海冰总浓度和多年浓度反演算法。利用Era-40大气参数廓线和海冰温度再分析资料,对微波辐射在大气-海洋-海冰系统中的辐射传输进行了数值积分。以北极谢巴试验结果为基础,对云中液态水含量和云界数据进行了建模。第一年和多年冰发射率的数值取自已发表的实验数据。计算得到的辐射计亮度温度值用于基于神经网络的理论算法开发。定义了新的天气过滤器。使用SSM/I数据和合成孔径雷达(SAR)图像,由冰专家分类,验证了算法在稳定冬季条件下的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neural-Network based algorithm for ice concentration retrievals from satellite passive microwave data
Present algorithms for observing the multiyear ice cover are not accurate in multiyear fraction calculations, which is a significant disadvantage of the present system of global ice monitoring considering the fact that multiyear ice is one of the key indicators of changes in the Arctic climate. In this research regionally differing Neural Networks (NN)-based algorithms for total and multiyear Arctic sea ice concentration retrievals from Special Sensor Microwave Imager (SSM/I) data are developed using closed scheme of the numerical experiment. Era-40 Reanalysis data on atmospheric parameter profiles and sea ice temperature are used for the numerical integration of the radiation transfer of the microwave emission in the Atmosphere-Ocean-Ice System. The data on cloud liquid water content and cloud boundaries are modeled basing on the results of Arctic SHEBA experiment. Numerical values for first year and multiyear ice emissivities are taken from published experimental data. The calculated radiometer brightness temperature values are used for NN-based theoretical algorithm development. New weather filter is defined. The algorithms are validated for stable winter conditions using collocated SSM/I data and Synthetic Aperture Radar (SAR) images, classified by an ice expert.
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