Abstract
Abstract. Dynamical models of various centres have shown in recent years seasonal prediction skill of the North Atlantic Oscillation (NAO). By filtering the ensemble members on the basis of statistical predictors, known as subsampling, it is possible to achieve even higher prediction skill. In this study the aim is to design a generalisation of the subsampling approach and establish it as a post-processing procedure. Instead of selecting discrete ensemble members for each year, as the subsampling approach does, the distributions of ensembles and statistical predictors are combined to create a probabilistic prediction of the winter NAO. By comparing the combined statistical–dynamical prediction with the predictions of its single components, it can be shown that it achieves similar results to the statistical prediction. At the same time it can be shown that, unlike the statistical prediction, the combined prediction has fewer years where it performs worse than the dynamical prediction. By applying the gained distributions to other meteorological variables, like geopotential height, precipitation and surface temperature, it can be shown that evaluating prediction skill depends highly on the chosen metric. Besides the common anomaly correlation (ACC) this study also presents scores based on the Earth mover's distance (EMD) and the integrated quadratic distance (IQD), which are designed to evaluate skills of probabilistic predictions. It shows that by evaluating the predictions for each year separately compared to applying a metric to all years at the same time, like correlation-based metrics, leads to different interpretations of the analysis.
Highlights
Seasonal prediction of the North Atlantic Oscillation (NAO) is a challenge
In a step we evaluate the yearly performance of the winter NAO (WNAO) prediction of the three different predictions (E, P and M) with the 1D-continuous-Earth mover’s distance (EMD) and 1D-continuous
The combined and statistical predictions demonstrate skill for the 1D-continuous-EMD score compared to a climatological prediction over the whole uncertainty range
Summary
Seasonal prediction of the North Atlantic Oscillation (NAO) is a challenge. During the year the NAO describes a high portion of the explained variability of the pressure field over the North Atlantic region and with it has a high influence on European weather. Predicting the WNAO on the seasonal scale is a longstanding aim of the community (Doblas-Reyes et al, 2003; Müller et al, 2005; Scaife et al, 2014) and various current seasonal prediction systems have demonstrated limited significant correlation skill for the WNAO (Butler et al, 2016). Dobrynin et al (2018) have shown that by combining statistical and dynamical predictions, a much higher significant correlation skill is achievable. The selected ensembles are used to create a new sub-selected ensemble mean, which has for the NAO index, and for many other variables and regions, a better prediction skill than the ensemble mean of all ensemble members
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