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Numerical Forecasts of the 15-16 June 2002 Southern Plains Mesoscale Convective System: Impact of Mesoscale Data and Cloud Analysis

机译:2002年6月15日至16日南部平原中尺度对流系统的数值预报:中尺度数据和云分析的影响

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High-resolution explicit forecasts using the Advanced Regional Prediction System (ARPS) of the 15-16 June 2002 mesoscale convective system (MCS) that occurred over the U.S. central and southern plains during the International H_2O Project (IHOP_2002) field experiment period are performed. The forecasts are designed to investigate the impact of mesoscale and convective-scale data on the initialization and prediction of an organized convective system. Specifically, the forecasts test the impact of special mesoscale surface and upper-air data collected by, but not necessarily specific to, IHOP_2002 and of level-II data from multiple Weather Surveillance Radar-1988 Doppler radars. The effectiveness of using 30-min assimilation cycles with the use of a complex cloud-analysis procedure and high-temporal-resolution surface data is also examined. The analyses and forecasts employ doubly nested grids, with resolutions of 9 and 3 km. Emphasis is placed on the solutions of the 3-km grid. In all forecasts, a strong, well-defined bow-shaped MCS is produced with structure and behavior similar to those of the observed system. Verification of these forecasts through both regular and phase-shifted equitable threat scores of the instantaneous composite reflectivity fields indicate that the use of the complex cloud analysis has the greatest positive impact on the prediction of the MCS, primarily by removing the otherwise needed "spinup" time of convection in the model. The impact of additional data networks is smaller and is reflected mainly in reducing the spinup time of the MCS too. The use of intermittent assimilation cycles appears to be quite beneficial when the assimilation window covers a time period when the MCS is present. Difficulties with verifying weather systems with high spatial and temporal intermittency are also discussed, and the use of both regular and spatially shifted equitable threat scores is found to be very beneficial in assessing the quality of the forecasts.
机译:使用2002年6月15日至16日在国际H_2O项目(IHOP_2002)现场试验期间发生在美国中部和南部平原的中尺度对流系统(MCS)的高级区域预报系统(ARPS)进行了高分辨率的显式预报。预测旨在调查中尺度和对流尺度数据对有组织对流系统的初始化和预测的影响。具体而言,这些预测测试了由IHOP_2002收集但不一定特定于IHSP_2002的特殊中尺度地面和高空数据以及来自多个Weather Surveillance Radar-1988多普勒雷达的II级数据的影响。还检查了使用30分钟的同化循环以及复杂的云分析程序和高时间分辨率的地表数据的有效性。分析和预测使用双重嵌套网格,分辨率分别为9 km和3 km。重点放在3公里网格的解决方案上。在所有预测中,均会生成具有与所观察系统相似的结构和行为的坚固,轮廓分明的弓形MCS。通过瞬时和复合反射率场的常规和相移公平威胁评分对这些预测的验证表明,使用复杂的云分析对MCS的预测具有最大的积极影响,主要是通过消除其他需要的“自旋”模型中的对流时间。附加数据网络的影响较小,并且也主要体现在减少MCS的启动时间上。当同化窗口覆盖存在MCS的时间段时,使用间歇性同化循环似乎非常有益。还讨论了验证具有高时空间歇性的天气系统的困难,并且发现使用规则和空间平移的公平威胁评分对评估预报的质量非常有用。

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