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首页> 外文期刊>ournal of the Meteorological Society of Japan >The Development of a Resolution-Independent Tropical Cyclone Detection Scheme for High-Resolution Climate Model Simulations
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The Development of a Resolution-Independent Tropical Cyclone Detection Scheme for High-Resolution Climate Model Simulations

机译:高分辨率气候模型模拟的与分辨率无关的热带气旋检测方案的开发

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?A novel method for detecting tropical cyclones in high-resolution climate model simulations is proposed herein and subjected to examination. The proposed method utilizes a two-dimensional scatterplot based on two quantities that represent the radial gradient and the tangential asymmetry of mid-to upper-level thickness around a simulated vortex. A comparison between the modeled and observed tropical cyclones using the nonhydrostatic regional climate model (NHRCM) with 20-km grid spacing under reanalysis-driven boundary conditions for one year revealed that no cyclones were missed and there was only one false alarm over a part of the western North Pacific near Japan. The simulated vortices were classified into two categories: tropical cyclones and extratropical cyclones. These two groups, having specific features, were also found in the results using present-day climate datasets, indicating that the tropical cyclones were reasonably distinguished from extratropical cyclones, although a one-by-one comparison could not, in principle, be conducted. Comparison of the results obtained from datasets with 5 km and 20 km grid spacing demonstrated that the detection scheme was only weakly dependent on the horizontal resolution. This dependence was further reduced by using the radial gradient over the outer radii instead of near the center of the vortex. The resolution-independent feature in this method is due to a procedure in which the tangential asymmetry of mid-to upper-level thickness is utilized instead of the relative vorticity at 850 hPa, often used in conventional schemes. This procedure allows the method to identify tropical cyclones without the need to determine a grid-dependent threshold. The method proposed here provides a useful tool for detecting tropical cyclones in high-resolution climate simulations.
机译:本文提出了一种在高分辨率气候模型模拟中检测热带气旋的新方法,并进行了检查。所提出的方法利用基于两个量的二维散点图,两个量代表径向涡度和围绕模拟涡旋的中高层厚度的切向不对称性。在重新分析驱动的边界条件下,使用非静水区域气候模型(NHRCM)在20 km网格间距下对模拟热带气旋和观测热带气旋进行了一年的比较,结果表明,没有错过任何热带气旋,并且在部分热带气旋中只有一个错误警报日本附近的北太平洋西部。模拟的涡旋分为两类:热带气旋和温带气旋。使用当前的气候数据集还可以在结果中找到这两组具有特定特征的数据,这表明热带气旋与温带气旋有一定的区别,尽管原则上不能进行一对一的比较。从网格间隔为5 km和20 km的数据集获得的结果进行比较,结果表明检测方案仅弱依赖于水平分辨率。通过使用外半径而不是涡旋中心附近的径向梯度,可以进一步降低这种依赖性。此方法中与分辨率无关的功能是由于使用了中上层厚度的切向不对称而不是通常在常规方案中使用的850 hPa相对涡度的过程所致。此过程使该方法无需确定依赖于网格的阈值即可识别热带气旋。本文提出的方法提供了一种用于在高分辨率气候模拟中检测热带气旋的有用工具。

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