A new nudging scheme for the current operational climate prediction system of the National Marine Environmental Forecasting Center of China

被引:0
作者
Xunshu Song
Xiaojing Li
Shouwen Zhang
Yi Li
Xinrong Chen
Youmin Tang
Dake Chen
机构
[1] Ministry of Natural Resources,State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography
[2] Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai),Environmental Science and Engineering
[3] University of Northern British Columbia,College of Oceanography
[4] National Marine Environmental Forecasting Center,Key Laboratory of Marine Hazards Forecasting of Ministry of Natural Resources
[5] Hohai University,undefined
[6] Hohai University,undefined
来源
Acta Oceanologica Sinica | 2022年 / 41卷
关键词
climate prediction system; initialization; prediction skill; ENSO; IOD;
D O I
暂无
中图分类号
学科分类号
摘要
A new nudging scheme is proposed for the operational prediction system of the National Marine Environmental Forecasting Center (NMEFC) of China, mainly aimed at improving El Niño-Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD) predictions. Compared with the origin nudging scheme of NMEFC, the new scheme adds a nudge assimilation for wind components, and increases the nudging weight at the subsurface. Increasing the nudging weight at the subsurface directly improved the simulation performance of the ocean component, while assimilating low-level wind components not only affected the atmospheric component but also benefited the oceanic simulation. Hindcast experiments showed that the new scheme remarkably improved both ENSO and IOD prediction skills. The skillful prediction lead time of ENSO was up to 11 months, 1 month longer than a hindcast using the original nudging scheme. Skillful prediction of IOD could be made 4–5 months ahead by the new scheme, with a 0.2 higher correlation at a 3-month lead time. These prediction skills approach the level of some of the best state-of-the-art coupled general circulation models. Improved ENSO and IOD predictions occurred across all seasons, but mainly for target months in the boreal spring for the ENSO and the boreal spring and summer for the IOD.
引用
收藏
页码:51 / 64
页数:13
相关论文
共 125 条
[1]  
Chen D(2004)Predictability of El Niño over the past 148 years Nature 428 733-736
[2]  
Cane M A(2000)Bias correction of an ocean-atmosphere coupled model Geophysical Research Letters 27 2585-2588
[3]  
Kaplan A(2015)Strong influence of westerly wind bursts on El Niño diversity Nature Geoscience 8 339-345
[4]  
Chen D(2020)An ensemble-based SST nudging method proposed for correcting the subsurface temperature field in climate model Acta Oceanologica Sinica 39 73-80
[5]  
Cane M A(1995)An improved procedure for EI Niño forecasting: Implications for predictability Science 269 1699-1702
[6]  
Zebiak S E(2017)Improved prediction of the Indian Ocean Dipole mode by use of subsurface ocean observations Journal of Climate 30 7953-7970
[7]  
Chen D(2014)The spatial patterns of initial errors related to the “winter predictability barrier” of the Indian Ocean Dipole Atmospheric and Oceanic Science Letters 7 406-410
[8]  
Lian T(2014)The “winter predictability barrier” for IOD events and its error growth dynamics: Results from a fully coupled GCM Journal of Geophysical Research: Oceans 119 8688-8708
[9]  
Fu C(2019)The extreme El Niño of 2015–2016: the role of westerly and easterly wind bursts, and preconditioning by the failed 2014 event Climate Dynamics 52 7339-7357
[10]  
Chen X(1989)The influence of ENSO on the summer climate change in China and its mechanism Advances in Atmospheric Sciences 6 21-32