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Sensitivity of tropical-cyclone models to the surface drag coefficient in different boundary-layer schemes

机译:不同边界层方案中热带气旋模型对表面阻力系数的敏感性

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The recent study of the sensitivity of tropical-cyclone intensification to the surface drag coefficient in a three-dimensional model by Montgomery et al. is extended to include a wind-speed-dependent drag coefficient and one of four boundary-layer parametrization schemes: the bulk, Blackadar, MRF and Gayno-Seaman schemes. The schemes are slightly modified to have the same drag coefficient formulation and the same constant exchange coefficients for sensible heat and moisture. Interest is focussed on the change in intensity of the azimuthally-averaged tangential wind speed and change in the low-level vortex structure when the standard value of the drag coefficient is halved or doubled. Changing the drag coefficient provides insight into unbalanced effects in the boundary layer and their impact on the vortex evolution and structure. The changes in vortex behaviour with changing drag coefficient are qualitatively similar for all schemes, the maximum intensification occurring for a value somewhere near the standard value of the drag coefficient. The interpretation given to explain this behaviour underlines the intrinsically unbalanced nature of the boundary-layer dynamics, although, for reasons discussed, a complete theory for the behaviour does not exist. The behaviour found is at odds with the predictions of Emanuel's (balance) theory for the maximum intensity of a tropical-cyclone, which predicts a monotonic decrease in intensity with the drag coefficient if the enthalpy exchange coefficient is held fixed. It is at odds also with a recent numerical study of the maximum intensity by Bryan and Rotunno. The study underscores the importance of boundary-layer dynamics in models for forecasting tropical-cyclone intensity and the need for care in choosing a boundary-layer scheme. However, it is not yet known which boundary-layer formulation is the most appropriate for this purpose, highlighting the need for a concerted research effort in this direction.
机译:Montgomery等人在三维模型中对热带气旋强化对表面阻力系数的敏感性的最新研究。扩展到包括风速相关的阻力系数和四个边界层参数化方案之一:体,Blackadar,MRF和Gayno-Seaman方案。对方案进行了稍微修改,以具有相同的阻力系数公式和相同的显热和水分常数交换系数。当阻力系数的标准值减半或加倍时,关注的重点是方位平均切向风速的强度变化和低水平涡旋结构的变化。改变阻力系数可以深入了解边界层中的不平衡效应及其对涡旋演变和结​​构的影响。对于所有方案,随着阻力系数的变化,涡旋行为的变化在质量上都是相似的,最大强度发生在阻力系数的标准值附近的某个值处。尽管出于所讨论的原因,不存在行为的完整理论,但为解释这种行为而做出的解释强调了边界层动力学的内在不平衡性质。发现的行为与伊曼纽尔(平衡)理论对热带气旋最大强度的预测相矛盾,该理论预测,如果焓交换系数保持不变,则随着阻力的增加,强度会单调降低。与布莱恩(Bryan)和罗图诺(Rotunno)最近对最大强度进行的数值研究也不一致。这项研究强调了边界层动力学在预测热带气旋强度的模型中的重要性以及在选择边界层方案时需要谨慎的必要性。但是,尚不知道哪种边界层配方最适合此目的,这凸显了朝此方向进行协调研究的必要性。

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