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Energy Budget Analysis for the Urban Effect on the Initiation of Heavy Rainfall Based on Meso-scale Simulation

机译:基于中尺度模拟的城市降雨引发的能源预算分析

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Urbanization greatly affects regional climates; one aspect that is affected is convective precipitation, which can cause serious damage to urban infrastructure. This study improves our understanding of urbanization effects on trigger mechanisms for local heavy rainfall. Convective clouds can develop during unstable conditions if the low moist air parcel is lifted to the free convection level. An energy budget analysis was performed to assess how urbanization contributes to the lifting of low-level moist air and triggers the development of a convective cloud. Energy budget equations for the kinematic, potential, and internal energies are presented, including terms for the energy exchange between the three energy types. Fine-scale simulations with a horizontal grid resolution of 1 km using the fifth-generation meso-scale model were used to examine the energy budget during the atmospheric destabilization process in the Tokyo metropolitan region. Numerical simulations successfully reproduced the local heavy rainfall observed in Tokyo on August 15, 2005. Before the heavy rain event occurred, the lower atmosphere was under latent instability conditions because of heating from the land surface. This study also discusses the energy transport from the surface to the lifted air parcels and clarifies the roles of the surface flux and low-level convergence kinematic energy in the trigger process, in which low-level air was lifted and merged with the convective cloud.
机译:城市化极大地影响了区域气候;受影响的一方面是对流降水,这可能对城市基础设施造成严重破坏。这项研究提高了我们对城市化对局部强降雨触发机制的影响的理解。如果将低湿空气包裹提升至自由对流水平,则在不稳定条件下会产生对流云。进行了能源预算分析,以评估城市化如何促进低空潮湿空气的产生并引发对流云的发展。给出了运动,势能和内部能量的能量预算方程,包括三种能量类型之间的能量交换术语。使用第五代中尺度模型在1 km的水平网格分辨率下进行了精细规模的模拟,以检验东京都会区大气不稳定过程中的能量收支。数值模拟成功地再现了2005年8月15日在东京观测到的局部强降雨。在强降雨事件发生之前,由于地面加热,低层大气处于潜在的不稳定条件下。这项研究还讨论了从表面到抬升的空气小包的能量传输,并阐明了表面通量和低水平收敛运动能在触发过程中的作用,在该过程中,低水平空气被抬升并与对流云合并。

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