Numerical Simulations of Derecho-producing Convective Systems

产生 Derecho 的对流系统的数值模拟

• 批准号: 0244846
• 负责人: David Stensrud
• 金额: $ 3.64万
• 依托单位: University of Oklahoma Norman Campus
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2003
• 资助国家: 美国
• 起止时间: 2003-07-01 至 2004-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0244846&HistoricalAwards=false
• 关键词: Numerical; Simulations; Derecho; producing; Convective

Understanding the environments and mechanisms responsible for the development and maintenance of widespread severe convective windstorms (derechos) remains an important research focus. These environments and mechanisms have been examined with idealized simulations of strong, line-oriented convection (squall lines), of which derecho-producing convective systems are a subset. These past studies emphasize the importance of environmental low-level wind shear in controlling the strength and longevity of squall lines. However, recent studies describing observed derecho environments have suggested that low-level shear is not a dominant factor. To address these issues, two main objectives have been defined: 1) produce a reasonably comprehensive set of horizontally non-homogeneous numerical simulations within the range of observed environments associated with derechos, and 2) produce an analogous set of horizontally homogeneous cloud-model simulations. This study will use a detailed classification of the observed wind and thermodynamics profiles in derecho environments as a baseline for the numerical simulations. The intellectual merit of this proposal is that the disparity between the results derived from observed derecho environments and those derived from idealized model simulations largely will be reconciled, and our knowledge of the physical mechanisms responsible for the development and maintenance of the line-oriented convection and the strong surface winds within these types of weather systems will be increased. The broader impacts are the improved forecasts of convective windstorms, resulting in enhanced public safety and economic benefits to commerce.

了解造成大范围强对流风暴发和维持的环境和机制仍然是一个重要的研究重点。这些环境和机制已经通过对强的、以线为导向的对流(咆哮线)的理想化模拟来检验，产生反回声的对流系统是其中的一个子集。这些过去的研究强调了环境低层风切变在控制斜风线的强度和寿命方面的重要性。然而，最近描述观测到的反回声环境的研究表明，低水平剪切不是主导因素。为了解决这些问题，已经确定了两个主要目标：1)在与德回波有关的观测环境范围内产生一组相当全面的水平非均匀数值模拟，以及2)产生一组类似的水平均匀云模型模拟。这项研究将使用DERECHO环境中观测到的风和热力学廓线的详细分类作为数值模拟的基线。这一建议的学术价值在于，从观测的DERECHO环境得出的结果与从理想化模式模拟得出的结果之间的差异将在很大程度上得到协调，并将增加我们对这些类型天气系统内以线为导向的对流和强地面风的发展和维持的物理机制的了解。更广泛的影响是改进了对流风暴的预报，从而提高了公共安全和商业的经济利益。