论文标题
替代合奏预测动态气候影响模型
Surrogate Ensemble Forecasting for Dynamic Climate Impact Models
论文作者
论文摘要
随着急性气候变化影响天气和气候变异性,对强大气候影响模型预测的需求增加,可以从中得出对影响的预测。这些预测的质量受气候驱动因素的限制,这些影响模型是非线性且自然界高度可变的。估计模型驱动因素的不确定性的一种方法是评估气候预测集合的分布。为了捕获与输入气候预测的分布相关的影响模型输出的不确定性,必须通过物理模型传播每个单独的预测合奏成员,这可能意味着高度计算成本。因此,希望训练一个替代模型,该模型可以预测气候驱动因素集团中输出分布的不确定性,从而减少资源需求。这项研究考虑了气候驱动的疾病模型,即利物浦疟疾模型(LMM),该模型预测了疟疾传播系数R0。通过模型传播了6个月范围的温度和降水的季节性集合预测,预测了传输时间序列的分布。输入数据和输出数据用于以随机森林分数回归(RFQR)模型和贝叶斯长短期记忆(BLSTM)神经网络的形式训练替代模型。比较预测性能,RFQR可以更好地预测单个集合成员的时间序列,而BLSTM提供了一种直接的方式来为所有集合成员构建组合分布。该方法的一个重要要素是,可以通过贝叶斯公式自然捕获气候预测集合的非正态分布。
As acute climate change impacts weather and climate variability, there is increased demand for robust climate impact model predictions from which forecasts of the impacts can be derived. The quality of those predictions are limited by the climate drivers for the impact models which are nonlinear and highly variable in nature. One way to estimate the uncertainty of the model drivers is to assess the distribution of ensembles of climate forecasts. To capture the uncertainty in the impact model outputs associated with the distribution of the input climate forecasts, each individual forecast ensemble member has to be propagated through the physical model which can imply high computational costs. It is therefore desirable to train a surrogate model which allows predictions of the uncertainties of the output distribution in ensembles of climate drivers, thus reducing resource demands. This study considers a climate driven disease model, the Liverpool Malaria Model (LMM), which predicts the malaria transmission coefficient R0. Seasonal ensembles forecasts of temperature and precipitation with a 6-month horizon are propagated through the model, predicting the distribution of transmission time series. The input and output data is used to train surrogate models in the form of a Random Forest Quantile Regression (RFQR) model and a Bayesian Long Short-Term Memory (BLSTM) neural network. Comparing the predictive performance, the RFQR better predicts the time series of the individual ensemble member, while the BLSTM offers a direct way to construct a combined distribution for all ensemble members. An important element of the proposed methodology is that accounting for non-normal distributions of climate forecast ensembles can be captured naturally by a Bayesian formulation.