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Ensemble lagged forecasts of a monsoon depression over India using a mesoscale model

机译:使用中尺度模型对印度季风低压的整体滞后预测

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摘要

A monsoon depression formed over the Bay of Bengal, India, during 27 July 1999 and crossed the east coast of India on 28 July 1999. The system caused copious rainfall over the east coast of India and adjacent regions and is investigated in this study using ensemble lagged methods with the Pennsylvania State University/National Center for Atmospheric Research (PSU/NCAR) Fifth Generation Mesoscale Model (MM5). Two sets of experiments are designed with five members of ensembles in each set starting at 12 UTC 25 July 1999 and at preceding times separated by 3 hour intervals. In the first experiment, the National Center for Environmental Prediction (NCEP) reanalysis data is utilized in the forecast of a coarse grid spacing domain and subsequent nest down to a finer (30 km) grid spacing domain. In the second experiment, the NCEP reanalysis data is directly utilized in the 30 kin domain as initial/boundary conditions. The results of the ensemble average of both experiments are compared with the analysis and observations. It is found that at the initial times of verification, the ensemble average of the sea level pressure field corresponding to the second experiment has a larger horizontal structure and is more closer to NCEP reanalysis. However at later times of verification, the ensemble average of sea level pressure field corresponding to the first experiment is found to be better. The area averaged 24 hour accumulated precipitation of all the ensemble members have higher values corresponding to the first experiment as compared to the second experiment. Also, the spread of the area averaged 24 hour accumulated precipitation of all the ensemble members with respect to their respective ensemble average are higher for the first experiment as compared to the second experiment. The results of the study would be useful to operational weather forecasting centers in India as it would provide them different evaluating ways to develop and test the importance of ensembles.
机译:1999年7月27日,在印度的孟加拉湾形成了季风低压区,并于1999年7月28日横越了印度的东海岸。该系统在印度的东海岸和邻近地区造成了大量的降雨,本研究利用系综进行了研究。宾夕法尼亚州立大学/国家大气研究中心(PSU / NCAR)第五代中尺度模型(MM5)提出了滞后方法。设计了两组实验,每组中有五个乐团成员,从1999年7月25日UTC开始,在之前的时间间隔为3小时。在第一个实验中,国家环境预测中心(NCEP)重新分析数据用于预测粗略的网格间距域,随后嵌套到更精细的网格间距域(30 km)。在第二个实验中,将NCEP重新分析数据直接用于30 kin域作为初始/边界条件。将两个实验的合计平均值的结果与分析和观察结果进行比较。发现在验证的初始时间,对应于第二次实验的海平面压力场的总体平均值具有较大的水平结构,并且更接近于NCEP重新分析。但是,在以后的验证中,发现与第一个实验相对应的海平面压力场的总体平均值更好。与第二个实验相比,所有集合的平均24小时累积降水面积具有更高的值。另外,与第二实验相比,第一实验的所有集合成员的平均24小时累积降水的面积相对于它们各自的集合平均的分布更大。研究结果将对印度的运营天气预报中心有用,因为它将为他们提供不同的评估方法,以开发和测试乐团的重要性。

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