Mitigating against the between-ensemble-member precipitation bias in a lagged sub-seasonal ensemble

IF 2.3 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Marion Mittermaier, Seshagiri Rao Kolusu, Joanne Robbins
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引用次数: 0

Abstract

The Met Office GloSea5-GC2 sub-seasonal-to-seasonal 40-member lagged ensemble consists of members who are up to 10 days different in age such that the between-ensemble-member bias is not internally consistent. Reforecasts tend to be used to convert these ensemble forecasts into anomalies from a normal state. These anomalies are however not that useful for applications where individual ensemble members are needed to drive downstream applications in the hazard and impact space. Here we explore whether there is a way of correcting for the within-ensemble bias without using reforecasts. An investigation into the individual daily precipitation distributions from the JJAS 2019 Indian monsoon season, stratified by forecast horizon, highlights how the distribution changes, and shows that the model distribution is markedly different to the observed. Initial results suggest that it could be better to use recent model forecast distribution(s) as the reference for adjusting the model rainfall accumulations as a function of lead day horizon, that is, not attempting to correct the members to a vastly different (observed) distribution shape, but a more subtle shift towards the model's best guess of reality, rather than reality itself, to remove the between-ensemble-member bias. A combination of Exponential and Generalized Pareto distributions are used for parametric quantile mapping to remove this internal ensemble bias using computationally efficient pre-computed lookup tables. Within- and out-of-sample results for the 2019 and 2020 monsoon seasons show that the method is effective in tightening precipitation gradients, with improvements in spread, accuracy and skill, especially for low accumulations.

Abstract Image

减少滞后亚季节集合中集合成员间降水偏差
英国气象局 GloSea5-GC2 分季节到季节的 40 个成员滞后集合包括年龄相差 10 天的成员,因此集合成员之间的偏差在内部并不一致。再预报往往用于将这些集合预报从正常状态转换为异常状态。然而,这些异常对于需要单个集合成员来推动灾害和影响空间下游应用的应用来说并不那么有用。在此,我们探讨是否有办法在不使用重新预测的情况下纠正集合内偏差。通过对 JJAS 2019 年印度季风季节的单个日降水量分布进行调查(按预报范围分层),突出了降水量分布的变化情况,并表明模式分布与观测到的降水量分布明显不同。初步结果表明,以最近的模式预报分布为参考,调整模式累积降雨量作为主导日范围的函数可能会更好,也就是说,不是试图将各成员修正为截然不同的(观测到的)分布形状,而是更微妙地转向模式对现实的最佳猜测,而不是现实本身,以消除集合成员之间的偏差。指数分布和广义帕累托分布的组合被用于参数量化映射,利用计算效率高的预计算查找表来消除这种内部集合偏差。2019 年和 2020 年季风季节的样本内和样本外结果表明,该方法能有效收紧降水梯度,并改善了分布、准确性和技能,尤其是在低累积量方面。
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来源期刊
Meteorological Applications
Meteorological Applications 地学-气象与大气科学
CiteScore
5.70
自引率
3.70%
发文量
62
审稿时长
>12 weeks
期刊介绍: The aim of Meteorological Applications is to serve the needs of applied meteorologists, forecasters and users of meteorological services by publishing papers on all aspects of meteorological science, including: applications of meteorological, climatological, analytical and forecasting data, and their socio-economic benefits; forecasting, warning and service delivery techniques and methods; weather hazards, their analysis and prediction; performance, verification and value of numerical models and forecasting services; practical applications of ocean and climate models; education and training.
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