基于仿真-实测知识迁移的裸地后向散射系数建模方法

      A method for modeling bare surface backscattering coefficients based on simulation-to-measurement knowledge transfer

      • 摘要: 裸地后向散射系数是微波雷达定量遥感建模与地表参数反演的关键基础。然而,受制于外场实测成本高、样本规模不足及观测条件复杂等因素,仅依赖实测数据的数据驱动建模容易陷入过拟合,且泛化能力严重受限;而物理模型基于理论假设与参数简化,又难以有效消除与真实观测间的系统偏差。针对上述问题,本文提出了一种基于仿真-实测知识迁移的裸地后向散射系数建模方法。该方法分为两阶段实施,首先利用物理模型在宽泛的地表参数(如粗糙度、土壤水分)空间内生成大规模仿真样本,将其作为源域数据预训练基准模型,使其充分学习地表物理量与散射响应间的非线性映射规律;随后,引入有限的真实外场测量样本作为目标域数据,通过模型参数微调完成从理论模拟向实测的知识迁移。实验结果表明,所提方法在小样本条件下的预测精度与鲁棒性均得到显著提升,可为裸地散射的高精度快速建模及后续遥感反演提供可靠的技术支撑。

         

        Abstract: The bare surface backscattering coefficient is a key foundation for quantitative remote sensing modeling and surface parameter inversion in microwave radar. However, due to factors such as the high cost of field measurements, limited sample sizes, and complex observation conditions, data-driven modeling that relies solely on measured data is prone to overfitting and suffers from severely limited generalization capabilities. Meanwhile, physical models, which are based on theoretical assumptions and parameter simplifications, struggle to effectively eliminate systematic biases between the models and actual observations. To address these issues, this paper proposes a modeling method for bare surface backscattering coefficients based on simulation-to-measurement knowledge transfer. The method is implemented in two stages. First, a physical model is used to generate a large-scale simulated dataset across a wide range of surface parameters (such as roughness and soil moisture). This dataset serves as a source-domain pre-training benchmark model, enabling it to fully learn the nonlinear mapping relationship between surface physical quantities and scattering responses. Subsequently, a limited number of real field measurement samples are introduced as target domain data. By employing a fine-tuning strategy, the method facilitates knowledge transfer from theoretical simulation to actual measurements. Experimental results reveal that the proposed method significantly improves prediction accuracy and robustness under small-sample conditions, providing reliable technical support for high-precision, rapid modeling of bare surface scattering and subsequent remote sensing inversion.

         

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