调查热带气旋探测系统之间的差异

Daniel Galea, Kevin Hodges, Bryan N. Lawrence
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摘要

热带气旋(TC)是一种重要现象;要了解它们的行为,就必须能够在模拟中探测到它们的存在。检测算法各不相同;在此,我们将一种基于深度学习的新型检测算法 TCDetect 与最先进的跟踪系统(TRACK)和观测数据集(IBTrACS)进行比较,为其在气候模拟中的潜在应用提供背景资料。先前的研究表明,TCDetect 具有良好的召回率,尤其是在飓风强度事件中。这里要解决的主要问题是系统结构在检测中的作用有多大。为了与对热带气旋的观测结果进行比较,有必要将探测技术应用于再分析。为此,我们使用了ERA-Interim,比较的一个关键部分是认识到ERA-Interim本身并不能完全反映观测结果。尽管存在这一局限,但应用于ERA-Interim的TCDetect和TRACK在很大程度上是一致的。此外,当只考虑飓风强度的热气旋时,TCDetect 和 TRACK 与 IBTrACS 的热气旋观测结果非常吻合。与 TRACK 一样,TCDetect 对强系统具有良好的召回率;但是,它发现了大量与较弱的 TC(即检测到具有飓风强度但实际上较弱的事件)和热带风暴相关的误报。由于 TCDetect 没有接受过定位热气旋的训练,因此使用了一种事后比较的方法。虽然这种方法并不总是成功,但在匹配物理空间中的路径和事件方面也取得了一些成功。对匹配结果的分析表明,北半球的结果最好,而且在大多数地区,无论使用哪种探测方法,探测结果在时间上都遵循相同的模式。
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Investigating differences between Tropical Cyclone detection systems
Tropical cyclones (TCs) are important phenomena; understanding their behaviour requires being able to detect their presence in simulations. Detection algorithms vary; here we compare a novel deep-learning-based detection algorithm, TCDetect, with a state-of-the-art tracking system (TRACK) and an observational dataset (IBTrACS) to provide context for potential use in climate simulations. Previous work has shown TCDetect has good recall, particularly for hurricane-strength events. The primary question addressed here is how much the structure of the systems plays a part in detection. To compare with observations of TCs, it is necessary to apply detection techniques to re-analysis. For this purpose, we use ERA-Interim, and a key part of the comparison is the recognition that ERA-Interim itself does not fully reflect the observations. Despite that limitation, both TCDetect and TRACK applied to ERA-Interim mostly agree with each other. Also, when considering only hurricane-strength TCs, TCDetect and TRACK correspond well with the TC observations from IBTrACS. Like TRACK, TCDetect has good recall for strong systems; however, it finds a significant number of false positives associated with weaker TCs (that is, events detected as having hurricane strength, but being weaker in reality) and extra-tropical storms. As TCDetect was not trained to locate TCs, a post-hoc method to perform comparisons was used. While this method was not always successful, some success in matching tracks and events in physical space was also achieved. The analysis of matches suggested the best results were found in the northern hemisphere and that in most regions the detections followed the same patterns in time no matter which detection method was used.
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