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Time-Expanded Sampling Approach for Ensemble Kalman Filter:Experiment Assimilation of Simulated Soundings 被引量:1

Time-Expanded Sampling Approach for Ensemble Kalman Filter:Experiment Assimilation of Simulated Soundings
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摘要 In the Ensemble Kalman Filter(EnKF) data assimilation-prediction system,most of the computation time is spent on the prediction runs of ensemble members.A limited or small ensemble size does reduce the computational cost,but an excessively small ensemble size usually leads to filter divergence,especially when there are model errors.In order to improve the efficiency of the EnKF data assimilation-prediction system and prevent it against filter divergence,a time-expanded sampling approach for EnKF based on the WRF(Weather Research and Forecasting) model is used to assimilate simulated sounding data.The approach samples a series of perturbed state vectors from Nb member prediction runs not only at the analysis time(as the conventional approach does) but also at equally separated time levels(time interval is △t) before and after the analysis time with M times.All the above sampled state vectors are used to construct the ensemble and compute the background covariance for the analysis,so the ensemble size is increased from Nb to Nb+2M×Nb=(1+2M)×Nb) without increasing the number of prediction runs(it is still Nb).This reduces the computational cost.A series of experiments are conducted to investigate the impact of △t(the time interval of time-expanded sampling) and M(the maximum sampling times) on the analysis.The results show that if t and M are properly selected,the time-expanded sampling approach achieves the similar effect to that from the conventional approach with an ensemble size of(1+2M)× Nb,but the number of prediction runs is greatly reduced. In the Ensemble Kalman Filter(EnKF) data assimilation-prediction system,most of the computation time is spent on the prediction runs of ensemble members.A limited or small ensemble size does reduce the computational cost,but an excessively small ensemble size usually leads to filter divergence,especially when there are model errors.In order to improve the efficiency of the EnKF data assimilation-prediction system and prevent it against filter divergence,a time-expanded sampling approach for EnKF based on the WRF(Weather Research and Forecasting) model is used to assimilate simulated sounding data.The approach samples a series of perturbed state vectors from Nb member prediction runs not only at the analysis time(as the conventional approach does) but also at equally separated time levels(time interval is △t) before and after the analysis time with M times.All the above sampled state vectors are used to construct the ensemble and compute the background covariance for the analysis,so the ensemble size is increased from Nb to Nb+2M×Nb=(1+2M)×Nb) without increasing the number of prediction runs(it is still Nb).This reduces the computational cost.A series of experiments are conducted to investigate the impact of △t(the time interval of time-expanded sampling) and M(the maximum sampling times) on the analysis.The results show that if t and M are properly selected,the time-expanded sampling approach achieves the similar effect to that from the conventional approach with an ensemble size of(1+2M)× Nb,but the number of prediction runs is greatly reduced.
出处 《Acta meteorologica Sinica》 SCIE 2011年第5期558-567,共10页
基金 Supported by the National Natural Science Foundation of China (40805044) Natural Science Foundation of Gansu Province(1010RJZA118) Fundmental Research Fund for Central Universities Science and Technology Development Program of China(lzujbky-2010-12)
关键词 ASSIMILATION ENKF time-expanded sampling assimilation EnKF time-expanded sampling
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  • 1龚建东,魏丽,陶士伟,赵刚,万丰.全球资料同化中误差协方差三维结构的准确估计与应用Ⅰ:观测空间协方差的准确估计[J].气象学报,2006,64(6):669-683. 被引量:18
  • 2顾震潮.天气数值预报中过去资料的使用问题[J].气象学报,1958,29(3):176-186.
  • 3顾震潮.作为初值问题的天气形势预报与由地面天气历史演变做预报的等值性[J].气象学报,1958,29(2):93-98.
  • 4[3]Qiu C J, Xu Q. A simple adjoint method of wind analysis for single-Doppler radar data. J Atmos Oceani Technal,1992, 9(5):588~598
  • 5[4]Laroche S, Zawadzki I. A variational analysis method for retrieval of three-dimensional wind field from single-Doppler radar data. J Atmos Sci, 1994, 51(18):2664~2684
  • 6[5]Shapiro A, Ellis S, Shaw J. Single-Doppler velocity retrievals with Phoenix II data: Clear air and microburst wind retrievals in the planetary boundary layer. J Atmos Sci, 1995,52(9):1265~1287
  • 7[6]Wolfsberg D G. Retrieval of three-dimensional wind and temperature fields from single-Doppler radar data:[Ph.D. thesis]. University of Oklahoma, 1987. 91pp
  • 8[7]Kapitza, H. Numerical experiments with the adjoint of a nonhydrostatic mesoscale model. Mon Wea Rev, 1991,119(12): 2993~3011
  • 9[8]Sun J, Flicher D, Lilly D. Recovery of three-dimensional wind and temperature fields from single-Doppler radar data. J Atmos Sci,1991,48(6):876~890
  • 10[9]Verlinde J, Cotton W R. Fitting microphysical observations of nonsteady convective clouds to a numerical model: An application of the adjoint technique of data assimilation to a kinematic model. Mon Wea Rev, 1993,121(10):2776~2793

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