利用深度学习改进短期热带气旋强度变化及其快速增强的预测

Jeong-Hwan Kim, Y. Ham, Daehyun Kim, Tim Li, Chen Ma
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摘要

预测热带气旋(TC)的强度仍然具有挑战性,尤其是当其强度发生快速变化时。本研究旨在开发一种卷积神经网络(CNN),用于 24 小时预报热带气旋强度变化及其在西太平洋上空的快速增强。该卷积神经网络模型(DeepTC)使用独特的损失函数--振幅焦点损失进行训练,以更好地捕捉大规模强度变化,如快速增强(RI)事件期间的强度变化。我们的研究表明,DeepTC 的性能优于业务预报,平均绝对误差更低(8.9%-10.2%),决定系数更高(31.7%-35%)。为了了解 DeepTC 在 RI 预测中的卓越表现,我们进行了闭塞敏感性分析,以量化每个预测因子的相对重要性。结果显示,纬度、先前强度变化、初始强度和垂直风切变等标量对成功预测 RI 起着至关重要的作用。此外,DeepTC 还利用相对湿度的三维分布来区分 RI 和非 RI,在 RI 事件中,对流层中低层的干湿度梯度更高,对流层高层的径向湿度梯度更陡。我们的研究表明,DeepTC 可以作为一个强大的工具,用于提高对 RI 的理解和 TC 强度预报的可靠性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improvement in forecasting short-term tropical cyclone intensity change and their rapid intensification using deep learning
Forecasting the intensity of a tropical cyclone (TC) remains challenging, particularly when it undergoes rapid changes in intensity. This study aims to develop a Convolutional Neural Network (CNN) for 24-hour forecasts of the TC intensity changes and their rapid intensifications over the western Pacific. The CNN model, the DeepTC, is trained using a unique loss function - an amplitude focal loss, to better capture large intensity changes, such as those during rapid intensification (RI) events. We showed that the DeepTC outperforms operational forecasts, with a lower mean absolute error (8.9-10.2%) and a higher coefficient of determination (31.7-35%). In addition, the DeepTC exhibits a substantially better skill at capturing RI events than operational forecasts. To understand the superior performance of the DeepTC in RI forecasts, we conduct an occlusion sensitivity analysis to quantify the relative importance of each predictor. Results revealed that scalar quantities such as latitude, previous intensity change, initial intensity, and vertical wind shear play critical roles in successful RI prediction. Additionally, DeepTC utilizes the three-dimensional distribution of relative humidity to distinguish RI cases from non-RI cases, with higher dry-moist moisture gradients in the mid-to-low troposphere and steeper radial moisture gradients in the upper troposphere showed during RI events. These relationship between the identified key variables and intensity change was successfully simulated by the DeepTC, implying that the relationship is physically reasonable. Our study demonstrates that the DeepTC can be a powerful tool for improving RI understanding and enhancing the reliability of TC intensity forecasts.
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