The Sensitivity of Supercell Cold Pools to the Lifting Condensation Level and the Predicted Particle Properties Microphysics Scheme

IF 2.8 3区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
S. Murdzek, Yvette P. Richardson, P. Markowski
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Abstract

Previous work found that cold pools in ordinary convection are more sensitive to the microphysics scheme when the lifting condensation level (LCL) is higher owing to a greater evaporation potential, which magnifies microphysical uncertainties. In the current study, we explore whether the same reasoning can be applied to supercellular cold pools. To do this, four perturbed-microphysics ensembles are run, with each using an environment with a different LCL. Similar to ordinary convection, the sensitivity of supercellular cold pools to the microphysics increases with higher LCLs, though the physical reasoning for this increase in sensitivity differs from a previous study. Using buoyancy budgets along parcel trajectories that terminate in the cold pool, we find that negative buoyancy generated by microphysical cooling is partially countered by a decrease in environmental potential temperatures as the parcel descends. This partial erosion of negative buoyancy as parcels descend is most pronounced in the low-LCL storms, which have steeper vertical profiles of environmental potential temperature in the lower atmosphere. When this erosion is accounted for, the strength of the strongest cold pools in the low-LCL ensemble is reduced, resulting in a narrower distribution of cold pool strengths. This narrower distribution is indicative of reduced sensitivity to the microphysics. These results suggest that supercell behavior and supercell hazards (e.g., tornadoes) may be more predictable in low-LCL environments.
超级暴风雪冷池对提升凝结水平和预测粒子特性微观物理方案的敏感性
之前的研究发现,当提升凝结水平(LCL)较高时,普通对流中的冷池对微观物理方案更加敏感,因为蒸发潜力更大,从而放大了微观物理的不确定性。在当前的研究中,我们探讨了同样的推理是否也能应用于超细胞冷池。为此,我们运行了四个扰动微观物理集合,每个集合都使用了不同的 LCL 环境。与普通对流类似,超细胞冷池对微物理的敏感性随着 LCL 的增大而增大,但这种敏感性增大的物理原因与之前的研究有所不同。通过使用以冷池为终点的包裹轨迹的浮力预算,我们发现微物理冷却产生的负浮力部分被包裹下降过程中环境潜在温度的降低所抵消。这种随着包裹下降而产生的部分负浮力侵蚀在低 LCL 风暴中最为明显,因为低层大气中的环境潜在温度垂直剖面更陡峭。如果考虑到这种侵蚀,低空低纬度组合中最强冷池的强度就会减弱,导致冷池强度分布变窄。这种较窄的分布表明对微物理的敏感性降低了。这些结果表明,在低 LCL 环境中,超级暴风圈行为和超级暴风圈危害(如龙卷风)可能更容易预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Monthly Weather Review
Monthly Weather Review 地学-气象与大气科学
CiteScore
6.40
自引率
12.50%
发文量
186
审稿时长
3-6 weeks
期刊介绍: Monthly Weather Review (MWR) (ISSN: 0027-0644; eISSN: 1520-0493) publishes research relevant to the analysis and prediction of observed atmospheric circulations and physics, including technique development, data assimilation, model validation, and relevant case studies. This research includes numerical and data assimilation techniques that apply to the atmosphere and/or ocean environments. MWR also addresses phenomena having seasonal and subseasonal time scales.
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