统计季节性预测的附加值

Climate Pub Date : 2024-06-04 DOI:10.3390/cli12060083
F. Krikken, G. Geertsema, Kristian Nielsen, Alberto Troccoli
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引用次数: 0

摘要

季节性气候预测有助于及时应对极端情况,如干旱或潮湿时期,这些时期会带来干旱、火灾和水资源管理挑战等额外风险。对极端温暖的夏季或寒冷的冬季及时发出警告,有助于为能源需求的增加做好准备。我们分析了三种不同方法产生的季节预报:(1) 仅基于观测数据的多线性统计预报系统;(2) 仅基于观测数据的非线性随机森林模型;(3) 基于过程的动态预报模型。统计模型是一个基于多元线性回归的经验系统,它被扩展到将前 3 个月的趋势纳入预测因子,并通过使用中间多元线性回归模型进一步减少了过度拟合。这使得厄尔尼诺现象的预报技能大大提高,特别是在春季。此外,印度洋偶极子(IOD)指数的预报技能也有所提高,尤其是在夏季和秋季。通过结合这三种预报方法,构建了一个混合多模式集合。不同的方法用于制作近地面气温季节预报(三个月平均值)和月累计降水量季节预报,提前期为一个月。与仅基于动力学模式的多模式集合相比,我们发现许多区域具有附加值。例如,在 6 月、7 月和 8 月的气温方面,北美、南美和欧洲的许多地区都观测到了附加值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Added Value of Statistical Seasonal Forecasts
Seasonal climate predictions can assist with timely preparations for extreme episodes, such as dry or wet periods that have associated additional risks of droughts, fires and challenges for water management. Timely warnings for extreme warm summers or cold winters can aid in preparing for increased energy demand. We analyse seasonal forecasts produced by three different methods: (1) a multi-linear statistical forecasting system based on observations only; (2) a non-linear random forest model based on observations only; and (3) process-based dynamical forecast models. The statistical model is an empirical system based on multiple linear regression that is extended to include the trend over the previous 3 months in the predictors, and overfitting is further reduced by using an intermediate multiple linear regression model. This results in a significantly improved El Niño forecast skill, specifically in spring. Also, the Indian Ocean dipole (IOD) index forecast skill shows improvements, specifically in the summer and autumn months. A hybrid multi-model ensemble is constructed by combining the three forecasting methods. The different methods are used to produce seasonal forecasts (three-month means) for near-surface air temperature and monthly accumulated precipitation seasonal forecast with a lead time of one month. We find numerous regions with added value compared with multi-model ensembles based on dynamical models only. For instance, for June, July and August temperatures, added value is observed in extensive parts of both Northern and Southern America, as well as Europe.
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