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Parametric Modeling of Transitioning Cyclone Wind Fields for Risk Assessment Studies in the Western North Pacific

机译:北太平洋西部风险评估研究的过渡气旋风场参数化模型

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Probabilistic risk assessment systems for tropical cyclone hazards rely on large ensembles of model simulations to characterize cyclones tracks, intensities, and the extent of the associated damaging winds. Given the computational costs, the wind field is often modeled using parametric formulations that make assumptions that are based on observations of tropical systems (e.g., satellite, or aircraft reconnaissance). In particular, for the Northern Hemisphere, most of the damaging contribution is assumed to be from the right of the moving cyclone, with the left-hand-side winds being much weaker because of the direction of storm motion. Recent studies have highlighted that this asymmetry assumption does not hold for cyclones undergoing extratropical transitions around Japan. Transitioning systems can exhibit damaging winds on both sides of the moving cyclone, with wind fields often characterized as resembling a horseshoe. This study develops a new parametric formulation of the extratropical transition phase for application in risk assessment systems. A compromise is sought between the need to characterize the horseshoe shape while keeping the formulation simple to allow for implementation within a risk assessment framework. For that purpose the tropical wind model developed by Willoughby et al. is selected as a starting point and parametric bias correction fields are applied to build the target shape. Model calibration is performed against a set of 37 extratropical transition cases simulated using the Weather Research and Forecasting Model. This newly developed parametric model of the extratropical transition phase shows an ability to reproduce wind field features observed in the western North Pacific Ocean while using only a restricted number of input parameters.
机译:热带气旋危害的概率风险评估系统依靠大量的模拟模型来表征气旋的轨迹,强度以及相关的破坏性风的程度。在给定计算成本的情况下,通常使用基于对热带系统(例如,卫星或飞机侦察)的观测进行假设的参数公式化对风场进行建模。特别是,对于北半球,大部分破坏贡献被假定为来自旋风分离器的右侧,由于风暴运动的方向,左侧风弱得多。最近的研究强调,这种不对称假设不适用于日本周围经历温带过渡的气旋。过渡系统在移动的旋风分离器的两侧都可能表现出破坏性的风,风场的特征通常类似于马蹄形。这项研究开发了一种新的温带过渡阶段的参数化公式,用于风险评估系统。在表征马蹄形形状的需求的同时,要使配方保持简单以允许在风险评估框架内实施,两者之间寻求折衷。为此,Willoughby等人开发了热带风模型。选择“ D”作为起点,并应用参数偏差校正字段以构建目标形状。针对使用天气研究和预报模型模拟的37个温带过渡案例进行模型校准。这种新近发展的温带过渡相参数模型显示出能够重现在北太平洋西部观测到的风场特征的能力,同时仅使用有限数量的输入参数。

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