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A triple-moment hail bulk microphysics scheme. Part Ⅱ: Verification and comparison with two-moment bulk microphysics

机译:三重矩冰雹体微物理学方案。第二部分:两步本体微物理学的验证与比较

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摘要

Microphysical parameterizations in numerical cloud models continue to grow in complexity as our capability to represent microphysical processes increases owing to greater knowledge of these processes as well as advances in computing power. In Part Ⅰ of this study, a new triple-moment bulk hail microphysics scheme (3MHAIL) that predicts the spectral shape parameter of the hail size distribution was presented and evaluated against lower order-moment schemes. In this paper, the 3MHAIL scheme is verified in simulations of a well-observed supercell storm that occurred over northwest Kansas on 29 June 2000 during the Severe Thunderstorm and Electrification and Precipitation Study (STEPS). Comparisons of the simulation results with the observations for this case, as well as with results of simulations using two different two-moment (2M) configurations of the RAMS microphysics schemes, suggest a significant improvement of the simulated storm structure and evolution is achieved with the 3MHAIL scheme. The generation of large hail and subsequent fallout in the simulation using 3MHAIL microphysics show particularly good agreement with surface hail reports for this storm as well as with previous studies of hail-producing supercell storms. On the other hand, the simulation with 2M microphysics produces only small hail aloft and virtually no hail at the surface, whereas a 2M version of the 3MHAIL scheme (with a fixed spectral shape parameter) produces unrealistically high amounts of large hail at low levels as a result of artificial shifts in the hail size spectra towards larger diameter hail during the melting process.
机译:由于对这些过程的更多了解以及计算能力的提高,数值云模型中的微物理参数化的复杂性不断提高,因为我们表示微物理过程的能力不断增强。在本研究的第一部分中,提出了一种新的三矩散装冰雹微物理方案(3MHAIL),该方案可预测冰雹尺寸分布的频谱形状参数,并针对低阶矩方案进行了评估。在本文中,通过对2000年6月29日发生在堪萨斯州西北部的强雷暴和电气化与降水研究(STEPS)上发生的观测良好的超级单体风暴的模拟,对3MHAIL方案进行了验证。将模拟结果与这种情况下的观察结果进行比较,以及使用RAMS微物理方案的两种不同的两矩(2M)配置进行的模拟结果进行比较,均表明模拟风暴结构得到了显着改善,并且使用3MHAIL方案。在使用3MHAIL微观物理学进行的模拟中,大冰雹的产生和随后的沉降显示出与该风暴的地面冰雹报告以及先前产生冰雹的超级单体风暴的研究特别一致。另一方面,使用2M微观物理学进行的模拟仅产生很小的冰雹,而表面几乎没有冰雹,而2M版本的3MHAIL方案(具有固定的光谱形状参数)在低水平时产生了不切实际的大量冰雹,如在融化过程中,冰雹尺寸谱的人为偏移导致了直径更大的冰雹。

著录项

  • 来源
    《Atmospheric research》 |2014年第12期|97-128|共32页
  • 作者

    A.M. Loftus; W.R. Cotton;

  • 作者单位

    Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA,Climate and Radiation and Laboratory, NASA Goddard Space Flight Center, 8800 Greenbelt Rd., Greenbelt, MD 20771, USA;

    Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Hail; Microphysics; Supercell convection; Cloud-resolving model;

    机译:冰雹;微观物理学;超单元对流;云解析模型;
  • 入库时间 2022-08-18 03:35:40

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