基于风云四号卫星的川藏铁路关键区强降水预报及关键因子特征

Heavy precipitation forecast in the key areas along the Sichuan-Xizang Railway based on FY-4 satellite and characteristics of critical factors

  • 摘要: 围绕川藏铁路关键区强降水预报、预警问题,基于2020—2024年夏季高时空分辨率的风云4号气象卫星观测数据和ERA5再分析资料,采用轻量级梯度提升机算法,构建了川藏铁路关键区分区域的强降水预报模型,并利用沙普利可加性解释方法(Shapley additive explanation,SHAP)做模型可解释性分析,深入剖析了关键预报因子的分布特征。结果表明:模型对关键区强降水预报命中率达0.76,临界成功指数为0.41,表现出良好的预报能力。分区域模型显示,川西地区模型表现优异,强降水命中率达0.83,临界成功指数为0.53,而青藏高原(简称高原)东南部地区模型命中率为0.69,临界成功指数为0.33,预报效果存在明显的区域差异。SHAP与统计分析显示,高原东南部强降水主要受反映中、高层水汽变化和云顶高度等的卫星亮温差因子(如BTD6.25−7.1、BTD13.5−10.7)主导,而热力不稳定参数(如对流有效位能、K指数)和低层垂直运动则是川西地区强降水的主要指示因子。强降水发生前60分钟关键卫星参数与物理量参数已具备显著的统计差异,关键卫星参数在降水前150分钟开始出现明显演变特征,为预警提供了定量参考。基于可解释机器学习方法,不仅能够提升强降水的客观预报能力,而且还有助于深化对区域强降水机制的理解,为川藏铁路关键区的防灾、减灾提供支撑。

     

    Abstract: Focusing on the forecasting and early warning of heavy precipitation in the key areas along the Sichuan-Xizang Railway, a heavy precipitation classification forecast model has been constructed for various subregions based on high spatiotemporal resolution Fengyun-4 (FY-4) satellite data and ERA5 reanalysis product for the summers of 2020—2024, combined with the Light Gradient Boosting Machine algorithm. The model's interpretability is analyzed using Shapley additive explanation (SHAP), and the distribution characteristics of key forecasting factors are analyzed. Results show that the model achieves a Critical Success Index (CSI) of 0.41 for heavy precipitation forecast in the key regions with a Probability Of Detection (POD) reaching 0.76, and demonstrates a strong forecasting capability. Regional model analysis indicates that the POD for heavy precipitation is 0.83 and the CSI is 0.53 in western Sichuan. The POD is 0.69 and the CSI is 0.33 in the southeastern region of the Qingzang Plateau, indicating significant regional differences in the forecasting. SHAP and statistical analysis show that heavy precipitation in the southeastern Qingzang Plateau is mainly dominated by satellite Brightness Temperature Difference (BTD) factors (such as BTD6.25−7.1 and BTD13.5−10.7) that reflect variations in mid- and upper-level water vapor and cloud top height, while thermal instability parameters (such as CAPE (Convective Available Potential Energy), K index) and low-level vertical motion are the main indicators for heavy precipitation in western Sichuan. 60 min prior to the occurrence of heavy precipitation, key satellite parameters and physical parameters already exhibited statistically significant differences. Satellite parameters begin to show notable evolutionary characteristics as early as 150 min prior to the precipitation, providing quantitative reference for early warning. Based on interpretable machine learning methods, it is possible to not only enhance the objective forecasting ability of heavy precipitation, but also deepen the understanding of regional heavy precipitation mechanisms. This study provides scientific support for disaster prevention and reduction along the key areas of the Sichuan-Xizang Railway.

     

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