SeisBench DAS: A machine learning framework for Distributed Acoustic Sensing
为解决DAS数据处理缺乏标准化问题,SeisBench DAS通过定义标准格式和利用PyTorch等工具,提供了一个机器学习框架以增强模型间的可比性和互操作性。
为解决DAS数据处理缺乏标准化问题,SeisBench DAS通过定义标准格式和利用PyTorch等工具,提供了一个机器学习框架以增强模型间的可比性和互操作性。
This study addresses the limitation of GRACE satellite observations, which provide terrestrial water storage (TWS) time series only since 2002 and thus hinder long-term climate analyses. To overcome this, the authors introduce a multivariate spatiotemporal graph neural network (MTGNN) for reconstructing monthly TWS anomalies back to 1940, leveraging daily ERA5 meteorological data—precipitation, evapotranspiration, and runoff. A novel interpretable hybrid adjacency matrix is constructed by integrating geographical distance with climate-driven lagged correlations. The model achieves high reconstruction accuracy, with Pearson correlation coefficients of 0.69 at the grid-cell scale and 0.94 at the basin scale, near-zero bias, and faithful representation of the spatial patterns associated with the 2015/16 El Niño and 2020/21 La Niña events. Notably, it attains performance comparable to existing methods while using only one-half to one-tenth of their input variables.
Neural networks often suffer significant performance degradation under distributional shifts—such as out-of-distribution generalization, spatiotemporal extrapolation, and cross-domain transfer—due to mismatches between training and deployment data distributions. To address this, we propose a conditional dynamic weight update framework. Its core innovation is a weight anomaly regression mechanism: sensitive weight change patterns induced by distribution shifts are identified via subset retraining; an interpretable regression predictor is then constructed to map input features to weight increments; finally, model parameters are conditionally extrapolated. The method integrates weight difference extraction, regression modeling, and extrapolation techniques, and is empirically validated on multi-source climate observation datasets. Across temporal, spatial, and cross-domain extrapolation tasks, it substantially improves prediction accuracy and robustness on out-of-distribution data, while preserving interpretability and practical applicability.
为解决DAS数据处理缺乏标准化问题,SeisBench DAS通过定义标准格式和利用PyTorch等工具,提供了一个机器学习框架以增强模型间的可比性和互操作性。
This study addresses the limitation of GRACE satellite observations, which provide terrestrial water storage (TWS) time series only since 2002 and thus hinder long-term climate analyses. To overcome this, the authors introduce a multivariate spatiotemporal graph neural network (MTGNN) for reconstructing monthly TWS anomalies back to 1940, leveraging daily ERA5 meteorological data—precipitation, evapotranspiration, and runoff. A novel interpretable hybrid adjacency matrix is constructed by integrating geographical distance with climate-driven lagged correlations. The model achieves high reconstruction accuracy, with Pearson correlation coefficients of 0.69 at the grid-cell scale and 0.94 at the basin scale, near-zero bias, and faithful representation of the spatial patterns associated with the 2015/16 El Niño and 2020/21 La Niña events. Notably, it attains performance comparable to existing methods while using only one-half to one-tenth of their input variables.
Neural networks often suffer significant performance degradation under distributional shifts—such as out-of-distribution generalization, spatiotemporal extrapolation, and cross-domain transfer—due to mismatches between training and deployment data distributions. To address this, we propose a conditional dynamic weight update framework. Its core innovation is a weight anomaly regression mechanism: sensitive weight change patterns induced by distribution shifts are identified via subset retraining; an interpretable regression predictor is then constructed to map input features to weight increments; finally, model parameters are conditionally extrapolated. The method integrates weight difference extraction, regression modeling, and extrapolation techniques, and is empirically validated on multi-source climate observation datasets. Across temporal, spatial, and cross-domain extrapolation tasks, it substantially improves prediction accuracy and robustness on out-of-distribution data, while preserving interpretability and practical applicability.