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arXiv 2012.15130stat.AP

估计热带气旋引起的海洋次表层热响应的时空方法

Spatio-temporal methods for estimating subsurface ocean thermal response to tropical cyclones

Addison J. Hu, Mikael Kuusela, Ann B. Lee, Donata Giglio, Kimberly M. Wood

AI总结:

本文提出一种整合季节估计、高斯过程与非参数回归的ANOVA时空框架,利用Argo浮标数据刻画热带气旋引起的全球海洋次表层热响应,揭示路径冷却与右侧增温。

摘要:

热带气旋(TCs)由海气之间的热交换驱动,对全球许多社区构成重大风险。准确刻画热带气旋过境后的次表层海洋热响应,对于精确的热带气旋强度预报以及理解热带气旋在全球气候系统中的作用至关重要。然而,由于海洋环境噪声高、时空数据固有的相关性、现场观测相对稀缺,以及热带气旋引起的信号与季节性信号的纠缠,这种刻画变得复杂。我们提出了一个解决这些困难的通用方法论框架,将季节平均场估计、高斯过程建模和非参数回归的现有技术整合到一个ANOVA分解模型中。重要的是,我们改进了以往的工作,正确处理了季节性,提供了严格的量化不确定性,并将时间视为连续变量,而不是产生按时间分箱的估计。该ANOVA模型使用来自Argo自主浮标阵列的现场次表层温度剖面,通过一个多步骤程序进行估计,该程序(1)刻画热带气旋季节期间上层海洋的季节性变化;(2)对温度观测中的变异性进行建模;(3)使用变异性估计拟合薄板样条,以考虑观测之间的异方差性和相关性。该样条拟合揭示了海洋对热带气旋过境的热响应。通过这一框架,我们获得了关于热带气旋与海洋在全球尺度上相互作用的新科学见解,包括沿热带气旋风暴路径的近表层和次表层冷却的三维刻画,以及路径右侧由混合引起的次表层增温。

英文摘要:

Tropical cyclones (TCs), driven by heat exchange between the air and sea, pose a substantial risk to many communities around the world. Accurate characterization of the subsurface ocean thermal response to TC passage is crucial for accurate TC intensity forecasts and for an understanding of the role that TCs play in the global climate system. However, that characterization is complicated by the high-noise ocean environment, correlations inherent in spatio-temporal data, relative scarcity of in situ observations, and the entanglement of the TC-induced signal with seasonal signals. We present a general methodological framework that addresses these difficulties, integrating existing techniques in seasonal mean field estimation, Gaussian process modeling, and nonparametric regression into an ANOVA decomposition model. Importantly, we improve upon past work by properly handling seasonality, providing rigorous uncertainty quantification, and treating time as a continuous variable, rather than producing estimates that are binned in time. This ANOVA model is estimated using in situ subsurface temperature profiles from the Argo fleet of autonomous floats through a multi-step procedure, which (1) characterizes the upper ocean seasonal shift during the TC season; (2) models the variability in the temperature observations; (3) fits a thin plate spline using the variability estimates to account for heteroskedasticity and correlation between the observations. This spline fit reveals the ocean thermal response to TC passage. Through this framework, we obtain new scientific insights into the interaction between TCs and the ocean on a global scale, including a three-dimensional characterization of the near-surface and subsurface cooling along the TC storm track and the mixing-induced subsurface warming on the track's right side.

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