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Areas beneath the relative operating characteristics (ROC) and relative operating levels (ROL) curves: Statistical significance and interpretation

统计的 事件(粒子物理) 统计 曼惠特尼U检验 统计假设检验 接收机工作特性 检验统计量 统计显著性 数学 口译(哲学) 计算机科学 物理 天体物理学 程序设计语言
作者
Simon J. Mason,Nicholas E. Graham
出处
期刊:Quarterly Journal of the Royal Meteorological Society [Wiley]
卷期号:128 (584): 2145-2166 被引量:719
标识
DOI:10.1256/003590002320603584
摘要

Abstract The areas beneath the relative (or receiver) operating characteristics (ROC) and relative operating levels (ROL) curves can be used as summary measures of forecast quality, but statistical significance tests for these areas are conducted infrequently in the atmospheric sciences. A development of signal‐detection theory, the ROC curve has been widely applied in the medical and psychology fields where significance tests and relationships to other common statistical methods have been established and described. This valuable literature appears to be largely unknown to the atmospheric sciences where applications of ROC and related techniques are becoming more common. This paper presents a survey of that literature with a focus on the interpretation of the ROC area in the field of forecast verification. We extend these foundations to demonstrate that similar principles can be applied to the interpretation and significance testing of the ROL area. It is shown that the ROC area is equivalent to the Mann–Whitney U ‐statistic testing the significance of forecast event probabilities for cases where events actually occurred with those where events did not occur. A similar derivation shows that the ROL area is equivalent to the Mann–Whitney U ‐statistic testing the magnitude of events with respect to whether or not an event has been forecast. Because the Mann–Whitney U ‐statistic follows a known probability distribution, under certain assumptions it can be used to define the statistical significance of ROC and ROL areas and for comparing the areas of competing forecasts. For large samples the significance of either measure can be accurately assessed using a normal‐distribution approximation. Copyright © 2002 Royal Meteorological Society

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