用改进的奇异向量法,找出影响气象预测误差的关键初始扰动方向。
Arnoldi Singular Vector perturbations for machine learning weather prediction
- 基于阿诺尔迪迭代构建误差增长子空间,无需线性化模型。
- 在24小时预报中发现从起点就快速增长的不稳定扰动模式。
- 适合用于机器学习气象预测的集合初始化,也适用于传统数值预报。
由于天气预报本身具有根本不确定性,可靠决策需要未来天气情景的概率信息。本文利用华为24小时Pangu天气机器学习模型,研究初始条件误差对机器学习气象预测(MLWP)的敏感性,采用一种特殊的奇异向量(SV)扰动方法。所提出的阿诺尔迪奇异向量(A-SV)方法无需线性或伴随模型,可应用于数值天气预报(NWP)和机器学习气象预测。通过迭代将预报模型作用于扰动状态,在给定优化时间窗口内观测误差增长,从而生成一个克雷洛夫子空间,该空间隐式基于矩阵算子,近似局部误差增长。每次迭代扩展子空间维度,其主导右奇异向量逐渐变为误差增长方向。实验表明,A-SV能有效识别出24小时Pangu模型中动态有意义的扰动模式,且误差从预报初期即开始增长。这些扰动描述了局部不稳定模态,可作为机器学习气象预测集合的初始化基础。由于A-SV从随机噪声扰动出发,算法将噪声转化为依赖参考状态的扰动,这一过程类似于通用扩散模型GenCast的去噪机制,本文简要讨论了二者的异同。
原文摘要 · Abstract (English)
Since weather forecasts are fundamentally uncertain, reliable decision making requires information on the likelihoods of future weather scenarios. We explore the sensitivity of machine learning weather prediction (MLWP) using the 24h Pangu Weather ML model of Huawei to errors in the initial conditions with a specific kind of Singular Vector (SV) perturbations. Our Arnoldi-SV (A-SV) method does not need linear nor adjoint model versions and is applicable to numerical weather prediction (NWP) as well as MLWP. It observes error growth within a given optimization time window by iteratively applying a forecast model to perturbed model states. This creates a Krylov subspace, implicitly based on a matrix operator, which approximates the local error growth. Each iteration adds new dimensions to the Krylov space and its leading right SVs are expected to turn into directions of growing errors. We show that A-SV indeed finds dynamically meaningful perturbation patterns for the 24h Pangu Weather model, which grow right from the beginning of the forecast rollout. These perturbations describe local unstable modes and could be a basis to initialize MLWP ensembles. Since we start A-SV from random noise perturbations, the algorithm transforms noise into perturbations conditioned on a given reference state - a process that is akin to the denoising process of the generic diffusion based ML model of GenCast, therefor we briefly discuss similarities and differences.
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