Advances in Earth Science

   

Microwave Remote Sensing of Snow Depth Based on Deep Learning Models and Wavelet Transform

Zhao Xinran1, 2, You Yuanhong1, 2*, Huang Chunlin3, 4, Tang Zhiguang5,Wang Zuo1, 2, Hou Jinliang3   

  1. (1. School of Geography and Tourism, Anhui Normal University, Wuhu Anhui 241002, China; 2. Anhui Provincial Engineering Research Center for Resources, Environment and Geographic Information Systems, Wuhu Anhui 241002, China; 3. Key Laboratory of Remote Sensing of Gansu Province, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; 4. School of Geomatics and Geoinformation,Lanzhou Jiaotong University, Lanzhou 730000, China; 5. National-Local Joint Engineering Laboratory of Geospatial Information Technology, Hunan University of Science and Technology, Xiangtan Hunan 411201, China)
  • About author:Zhao Xinra, research areas include snow depth retrieval, deep learning, and multi-source remote sensing data assimilation.E-mail: xinranzhao@anhu.edu.cn
  • Supported by:
    Project supported by the National Natural Science Foundation of China (Grant No. 42130113, 42371398); the Open Fund of Hunan Provincial Key Laboratory of Geo-Information Engineering in Surveying, Remote Sensing and Information Engineering (Grant No. E22405).

Zhao Xinran, You Yuanhong, Huang Chunlin, Tang Zhiguang, Wang Zuo, Hou Jinliang. Microwave Remote Sensing of Snow Depth Based on Deep Learning Models and Wavelet Transform[J]. Advances in Earth Science, DOI: 10.11867/j.issn.1001-8166.2026.010.

Abstract: Accurate retrieval of snow depth from passive microwave observations remains a major challenge because of the pronounced nonlinearity between microwave brightness temperature and snow physical properties, which is further modulated by complex terrain and the temporal evolution of snowpacks. Conventional retrieval approaches, including physically based radiative transfer models, are often constrained by high computational costs and strong sensitivity to uncertain input parameters, resulting in degraded performance under heterogeneous snow conditions and across different snow climate regimes. To overcome these limitations, this study develops a passive microwave snow depth retrieval model that integrates wavelet transform with a residual convolutional neural network (Wavedec-ResNet-CNN) to better represent multi-scale features and complex nonlinear relationships. Specifically, the wavelet transform is applied to multi-frequency brightness temperature observations to extract scale-dependent information, allowing the model to capture both large-scale snow depth variability and localized perturbations associated with rapid snow accumulation and melt processes. The resulting multi-scale features are then ingested into a residual convolutional neural network, in which residual connections facilitate deep feature propagation and enhance nonlinear fitting capability while mitigating performance degradation in deep architectures. The proposed model is evaluated using representative groundbased stations spanning different snow climate classes in the Northern Hemisphere to assess its applicability under diverse snow conditions at the site scale. Model performance is quantified using multiple statistical metrics, including root mean square error (RMSE), correlation coefficient (R), mean bias, and Nash-Sutcliffe efficiency (NSE), and is benchmarked against conventional convolutional neural network and residual convolutional neural network models. The results show that the Wavedec-ResNet-CNN achieves an RMSE of 0.23 m, an R of 0.93, a mean bias of 0.01 m, and an NSE of 0.86, indicating consistent improvements over the reference deep learning models across all evaluation metrics. Additional analyses demonstrate that the proposed model outperforms traditional deep learning approaches across a wide range of snow depths, with particularly notable gains during periods of deep snow accumulation and rapid snow depth changes. Furthermore, compared with existing snow depth retrieval products, the model exhibits enhanced temporal responsiveness and improved spatial transferability across different snow climate types, highlighting its potential for robust passive microwave snow depth monitoring in regions with diverse snow regimes.
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