不同天气控制下微物理不确定性条件对初始和边界条件不确定性的影响

T. Matsunobu, C. Keil, C. Barthlott
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引用次数: 2

摘要

摘要采用允许对流的ICON-D2 (ICOsahedral Non-hydrostatic)模型,量化了初始条件和边界条件不确定性(IBC)存在时,云凝结核(CCN)浓度的单个和组合不确定性以及云滴大小分布(CDSD)的形状参数对对流预报的相对影响。我们对代表德国不同天气强迫情况的五个实际案例进行了180个成员的整体模拟,并在不同的时空尺度上检查了降水的变化。在弱天气控制期间,综合微物理不确定性对日平均面积降水的相对影响约占业务IBC不确定性引起的变率的三分之一。综合微物理扰动的影响超过单个CCN或CDSD扰动的影响,并且在弱控制期间是其两倍。在弱强迫条件下,IBC和微物理不确定性的组合通过将预报分布的尾部延长5%来影响单个成员的日空间平均降雨量的极值。在强强迫情况下,这些反应相对不敏感。逐时降雨率空间变异性的目测和客观分析表明,atibc和微物理不确定性对降水预报空间变异性的影响不同。微物理扰动会轻微移动对流单体,但会影响降水强度,而IBC扰动会在弱控制期间打乱对流的位置。云和雨水含量对微物理不确定性比降水更敏感,对天气控制的依赖性较小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The impact of microphysical uncertainty conditional on initial and boundary condition uncertainty under varying synoptic control
Abstract. The relative impact of individual and combined uncertainties of cloud condensation nuclei (CCN) concentration and the shape parameter of the cloud droplet size distribution (CDSD) in the presence of initial and boundary condition uncertainty (IBC) on convection forecasts is quantified using the convection-permitting model ICON-D2 (ICOsahedral Non-hydrostatic). We performed 180-member ensemble simulations for five real case studies representing different synoptic forcing situations over Germany and inspected the precipitation variability on different spatial and temporal scales. During weak synoptic control, the relative impact of combined microphysical uncertainty on daily area-averaged precipitation accounts for about one-third of the variability caused by operational IBC uncertainty. The effect of combined microphysical perturbations exceeds the impact of individual CCN or CDSD perturbations and is twice as large during weak control. The combination of IBC and microphysical uncertainty affects the extremes of daily spatially averaged rainfall of individual members by extending the tails of the forecast distribution by 5 % in weakly forced conditions. The responses are relatively insensitive in strong forcing situations. Visual inspection and objective analysis of the spatial variability in hourly rainfall rates reveal that IBC and microphysical uncertainties alter the spatial variability in precipitation forecasts differently. Microphysical perturbations slightly shift convective cells but affect precipitation intensities, while IBC perturbations scramble the location of convection during weak control. Cloud and rainwater contents are more sensitive to microphysical uncertainty than precipitation and less dependent on synoptic control.
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