期刊文献+

Application and Characteristic Analysis of the Moist Singular Vector in GRAPES-GEPS 被引量:3

下载PDF
导出
摘要 The singular vector(SV)initial perturbation method can capture the fastest-growing initial perturbation in a tangent linear model(TLM).Based on the global tangent linear and adjoint model of GRAPES-GEPS(Global/Regional Assimilation and Prediction System-Global Ensemble Prediction System),some experiments were carried out to analyze the structure of the moist SVs from the perspectives of the energy norm,energy spectrum,and vertical structure.The conclusions are as follows:The evolution of the SVs is synchronous with that of the atmospheric circulation,which is flowdependent.The moist and dry SVs are located in unstable regions at mid-to-high latitudes,but the moist SVs are wider,can contain more small-and medium-scale information,and have more energy than the dry SVs.From the energy spectrum analysis,the energy growth caused by the moist SVs is reflected in the relatively small-scale weather system.In addition,moist SVs can generate perturbations associated with large-scale condensation and precipitation,which is not true for dry SVs.For the ensemble forecasts,the average anomaly correlation coefficient of large-scale circulation is better for the forecast based on moist SVs in the Northern Hemisphere,and the low-level variables forecasted by the moist SVs are also improved,especially in the first 72 h.In addition,the moist SVs respond better to short-term precipitation according to statistical precipitation scores based on 10 cases.The inclusion of the large-scale condensation process in the calculation of SVs can improve the short-term weather prediction effectively.
出处 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2020年第11期1164-1178,共15页 大气科学进展(英文版)
基金 the National Key R&D Program of China(Grant Nos.2017YFC1502102 and 2017YFC1501803).
  • 相关文献

参考文献4

二级参考文献37

  • 1陈德辉,沈学顺.新一代数值预报系统GRAPES研究进展[J].应用气象学报,2006,17(6):773-777. 被引量:150
  • 2Bishop C H, Toth Z. 1999. Ensemble transformation and adaptiveobservations. 3 Atmos Sci,56(11) : 1748-1765.
  • 3Bowler N E. 2006. Comparison of perturbation strategies on a sim-ple model. Tellus, 58A: 538-548.
  • 4Buizza R. 1994. Localization of optimal perturbations using a projec-tion operator. Quart J Roy Meteor Soc, 120(520) : 1647-1681.
  • 5Buizza R, Palmer T N. 1995. The singular-vector structure of theatmospheric global circulation. J Atmos Sci, 52(9) ? 1434-1456.
  • 6Buizza R. 1995. Optimal perturbation time evolution and sensitivityof ensemble prediction to perturbation amplitude. Quart J RoyMeteor Soc, 121(527): 1705-1738.
  • 7Buizza R, Gelaro R, Molteni F, et al. 1997. The impact of in-creased resolution on predictability studies with singular vec-tors. Quart J Roy Meteor Soc, 123(543) : 1007-1033.
  • 8Buizza R, Houtekamer P L,Toth Z,et al. 2005. A comparison ofthe ECMWF,MSC,and NCEP global ensemble prediction sys-tems. Mon Wea Rev, 133(5): 1076-1097.
  • 9Ehrendorfer M. 1994a. The Liouville equation and its potential use-fulness for the prediction of forecast skill,Part I : Theory.Mon Wea Rev, 122(4): 703-713.
  • 10Ehrendorfer M. 1994b. The Liouville equation and its potential use-fulness for the prediction of forecast skill,part U : applications.Mon Wea Rev, 122(4) : 714-728.

共引文献49

同被引文献26

引证文献3

二级引证文献9

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部