Green Benjamin W, Sun Shan, Bleck Rainer, Benjamin Stanley G, Grell Georg A
Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, and NOAA/Earth System Research Laboratory/Global Systems Division, Boulder, Colorado.
NASA Goddard Institute for Space Studies, New York, New York, and Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, and NOAA/Earth System Research Laboratory/Global Systems Division, Boulder, Colorado.
Mon Weather Rev. 2017 Jul;145(7):2555-2574. doi: 10.1175/MWR-D-16-0419.1. Epub 2017 Jun 15.
Monthlong hindcasts of the Madden-Julian oscillation (MJO) from the atmospheric Flow-following Icosahedral Model coupled with an icosahedral-grid version of the Hybrid Coordinate Ocean Model (FIM-iHYCOM), and from the coupled Climate Forecast System, version 2 (CFSv2), are evaluated over the 12-yr period 1999-2010. Two sets of FIM-iHYCOM hindcasts are run to test the impact of using Grell-Freitas (FIM-CGF) versus simplified Arakawa-Schubert (FIM-SAS) deep convection parameterizations. Each hindcast set consists of four time-lagged ensemble members initialized weekly every 6 h from 1200 UTC Tuesday to 0600 UTC Wednesday. The ensemble means of FIM-CGF, FIM-SAS, and CFSv2 produce skillful forecasts of a variant of the Real-time Multivariate MJO (RMM) index out to 19, 17, and 17 days, respectively; this is consistent with FIM-CGF having the lowest root-mean-square errors (RMSEs) for zonal winds at both 850 and 200 hPa. FIM-CGF and CFSv2 exhibit similar RMSEs in RMM, and their ensemble mean extends skillful RMM prediction out to 21 days. Conversely, adding FIM-SAS-with much higher RMSEs-to CFSv2 (as a multimodel ensemble) or FIM-CGF (as a ensemble) yields either little benefit, or even a degradation, compared to the better single-model ensemble mean. This suggests that multiphysics/multimodel ensemble mean forecasts may only add value when the individual models possess similar skill and error. An atmosphere-only version of FIM-CGF loses skill after 11 days, highlighting the importance of ocean coupling. Further examination reveals some sensitivity in skill and error metrics to the choice of MJO index.
利用大气跟随正二十面体模型与混合坐标海洋模型的正二十面体网格版本(FIM-iHYCOM)以及气候预测系统第2版(CFSv2),对1999年至2010年这12年期间的马登-朱利安振荡(MJO)进行了为期一个月的后报评估。运行了两组FIM-iHYCOM后报,以测试使用格雷尔-弗雷塔斯(FIM-CGF)与简化的荒川-舒伯特(FIM-SAS)深对流参数化的影响。每个后报集由四个时间滞后的集合成员组成,从协调世界时周二12:00到协调世界时周三06:00每6小时每周初始化一次。FIM-CGF、FIM-SAS和CFSv2的集合平均值分别对实时多变量MJO(RMM)指数的一个变体产生了长达19天、17天和17天的有效预报;这与FIM-CGF在850和200百帕的纬向风具有最低均方根误差(RMSE)一致。FIM-CGF和CFSv2在RMM中表现出相似的RMSE,并且它们的集合平均值将有效的RMM预测延长到了21天。相反,将RMSE高得多的FIM-SAS添加到CFSv2(作为多模型集合)或FIM-CGF(作为集合)中,与更好的单模型集合平均值相比,要么益处不大,甚至会导致预报性能下降。这表明,只有当各个模型具有相似的技能和误差时,多物理/多模型集合平均预报才可能增加价值。仅大气版本的FIM-CGF在11天后失去了技能,凸显了海洋耦合的重要性。进一步研究发现,技能和误差指标对MJO指数的选择存在一定敏感性。