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爬绕流对四川盆地一次盛夏暴雨的动热力和水汽输送作用

Dynamic heat and water vapor transport effects of a midsummer rainstorm event in the Sichuan Basin under the impact of flow over and flow around

  • 摘要: 四川盆地四周地形多样,产生的爬流与绕流运动十分显著,目前对于爬绕流运动对动热力和水汽输送作用的研究仍存在不足。本文基于ERA5再分析资料和GPM卫星降水产品,运用爬绕流分解方程组与水汽通量散度、涡度方程及螺旋度方程对2023年7月12—13日四川盆地暴雨过程中的爬绕流运动在动力、热力及水汽输送中的作用进行了诊断分析。结果表明:(1) 暴雨初生期,爬流平流项与绕流散度项协同驱动正涡度增长;强盛期,扭转项激增主导涡度增强而绕流平流项的抑制作用明显;结束期,持续强抑制的爬流散度项和绕流平流项共同作用导致正涡度快速衰减。(2) 整个过程中,绕流和爬流散度项对涡度的贡献相反并占据主导地位,前者始终促进涡度发展,而后者持续抑制涡度增长,在正负贡献上分别占比64.6%和44.6%。(3) 爬流的水汽和热力螺旋度驱动中低层水汽和热量向上输送;绕流的水汽和热力螺旋度提升低层向中层水汽输送的效率和强度并通过抽吸低层高温空气,不断增强中层位势不稳定,最终通过不稳定能量的释放产生暴雨。本文通过对爬绕流运动的定量解析,能够为四川盆地山区暴雨的预报提供理论参考。

     

    Abstract: The Sichuan Basin is surrounded by complex topography, resulting in significant over flows and around flows. However, research on the roles of these flows in term of dynamic, thermodynamic processes and water transport remains insufficient. Based on the ERA5 reanalysis data and GPM satellite precipitation products, this study presents a diagnostic analysis of the roles of topographically forced over flows and around flows in heat and water vapor transport during a heavy rainstorm in the Sichuan Basin from July 12 to 13, 2023, using a set of decomposition equations for the over and around flows together with equations of water vapor flux divergence, vorticity and helicity. The results are as follows. (1) The over flow advection term and around flow divergence term synergistically drive positive vorticity growth during the initial stage of the rainstorm; In the mature stage, surge of the tilting term dominates vorticity enhancement while the suppressive effect of the around flow advection term is pronounced. During the dissipation stage, the persistently strongly suppressive divergence term of the over flow and advection term of the around flow jointly cause rapid decay of positive vorticity. (2) Throughout the process, the divergence terms of the around flow and over flow exhibit opposing contributions to vorticity, with the former consistently promoting vorticity development (64.6%) and the latter continuously inhibiting it (44.6%). (3) The moisture and thermal helicity of the over flow drive upward transport of water vapor and heat from the middle and lower troposphere; the moisture and thermal helicity of the around flow enhance the moisture transport from the lower to middle troposphere, while they continuously intensify mid-level potential instability by pumping high-temperature air from lower troposphere. Ultimately, rainstorms are generated through the release of unstable energy. This quantitative analysis of the over and around flows provides a theoretical reference for forecasting mountain-triggered rainstorms in the Sichuan Basin.

     

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