| 基于非静力模式物理扰动的中尺度集合预报试验 |
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| 引用本文： | 谭燕,陈德辉.基于非静力模式物理扰动的中尺度集合预报试验[J].应用气象学报,2007,18(3):396-406. |
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| 作者姓名： | 谭燕 陈德辉 |
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| 作者单位： | 中国气象科学研究院, 北京 100081 |
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| 基金项目： | 国家自然科学基金;国家重点基础研究发展计划(973计划) |
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| 摘 要： | 以GRAPES中尺度有限区模式作为试验模式, 从模式的不确定性方面来构造中尺度的集合预报, 重点考虑物理因子与初始条件的扰动作用。针对2004年7月10日北京城区的突发性暴雨过程进行了36 h的集合预报试验。结果表明:GRAPES模式可有效地捕捉到中尺度过程的信息; 中尺度集合预报是可行的, 可改进中尺度暴雨过程落区、强度的预报; 不同集合方案的预报结果各不相同, 同一方案各个成员的预报结果也有差异, 即存在适宜的离散度; 在离散度分析中发现在北京附近存在一个明显大值区, 且在大气中低层的垂直结构表现出一致性, 表明这一区域的预报不确定性很大。从集合检验结果中得到:单纯考虑模式物理扰动来构造中尺度集合预报系统有一定难度, 当加入初始场不确定信息后, 同时考虑模式的不确定性和初始场的不确定性, 有助于捕捉更多的中尺度系统的不确定信息, 有助于构造更为有效的中尺度集合预报系统。
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| 关 键 词： | 中尺度集合预报 不确定性 初始扰动 物理扰动 |
| 收稿时间： | 2005-10-08 |
| 修稿时间： | 2005-10-082006-09-18 |
Meso-scale Ensemble Forecasts on Physical Perturbation Using a Non-hydrostatic Model |
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| Tan Yan,Chen Dehui.Meso-scale Ensemble Forecasts on Physical Perturbation Using a Non-hydrostatic Model[J].Quarterly Journal of Applied Meteorology,2007,18(3):396-406. |
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| Authors: | Tan Yan Chen Dehui |
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| Institution: | Chinese Academy of Meteorological Sciences, Beijing 100081 |
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| Abstract: | The past decade has seen increasing interest in ensemble methods for operational numerical weather prediction.Ensemble forecasting is motivated by the recognition that numerical predictions always contain both initial condition uncertainties and numerical model uncertainties.It is traditionally desirable to use an ensemble method focused mainly on uncertainties in the initial conditions for the medium range forecasts.Encouraged by the success of global medium-range ensemble forecast,investigations are made in examining the short-range ensemble forecast(SREF) with meso-scale models.It is found that the ensemble approach could also improve short-range weather forecasts,especially the forecasting of quantitative precipitation,meso-scale convective systems.However,it is still challenging for meso-scale ensemble forecast due to the difficulty to generate a well spreading perturbation which triggers meso-scale and convective processes in a short time. Motivated by the previous studies on meso-scale ensemble forecasts,a meso-scale ensemble forecast system based on a limited area non-hydrostatic meso-scale NWP model(GRAPES-Meso) is carried out,to construct meso-scale ensemble,especially considering the perturbation of the physical sensitive factors and the initial conditions.As a preliminary step,the objective of the study is to understand the impact of model physics uncertainties on predicting extreme precipitation events using meso-scale ensemble forecast.A flash flood case on July 10,2004 in Beijing is particularly chosen for the study of a 36 h meso-scale ensemble forecast.The "7.10" flash flood causes a high impact on traffic and open air activities because of the failure of the forecast.In particular,the uncertainties in convective parameterization schemes are focused on.The members of SREF are constructed by specifying the closure assumptions,triggering parameters and precipitation efficiency.Meanwhile meso-scale ensemble forecast is constructed using multi-physical parameterizations and the uncertainty of initial condition is added using the Monte Carlo method. The verification results show some characteristics of the meso-scale system could be captured by GRAPES and meso-scale ensemble is feasible to improve on the forecast site and the forecast intensify of the precipitation.Different ensemble experiment has different result,even in the same experiment,members differ with each other,and it means there is an appropriate spread among members.In spread analysis,from the surface to the middle-level of troposphere there is a maximum value area in Beijing,i.e.,this area has large uncertainties.Meanwhile it is found that it's difficult to construct ensemble system only considering model uncertainties,if initial condition uncertainties are added,the results are preliminary but encouraging,it is helpful to capture more meso-scale information and construct more effective meso-scale ensemble system. |
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| Keywords: | meso-scale ensemble forecast uncertainty initial perturbation physical perturbation |
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