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DOI10.1007/s00382-018-4217-0
Contribution of tropical instability waves to ENSO irregularity
Holmes R.M.; McGregor S.; Santoso A.; England M.H.
发表日期2019
ISSN0930-7575
起始页码1837
结束页码1855
卷号52期号:2020-03-04
英文摘要Tropical instability waves (TIWs) are a major source of internally-generated oceanic variability in the equatorial Pacific Ocean. These non-linear phenomena play an important role in the sea surface temperature (SST) budget in a region critical for low-frequency modes of variability such as the El Niño–Southern Oscillation (ENSO). However, the direct contribution of TIW-driven stochastic variability to ENSO has received little attention. Here, we investigate the influence of TIWs on ENSO using a 1 / 4 ∘ ocean model coupled to a simple atmosphere. The use of a simple atmosphere removes complex intrinsic atmospheric variability while allowing the dominant mode of air−sea coupling to be represented as a statistical relationship between SST and wind stress anomalies. Using this hybrid coupled model, we perform a suite of coupled ensemble forecast experiments initiated with wind bursts in the western Pacific, where individual ensemble members differ only due to internal oceanic variability. We find that TIWs can induce a spread in the forecast amplitude of the Niño 3 SST anomaly 6-months after a given sequence of WWBs of approximately ±45% the size of the ensemble mean anomaly. Further, when various estimates of stochastic atmospheric forcing are added, oceanic internal variability is found to contribute between about 20 % and 70 % of the ensemble forecast spread, with the remainder attributable to the atmospheric variability. While the oceanic contribution to ENSO stochastic forcing requires further quantification beyond the idealized approach used here, our results nevertheless suggest that TIWs may impact ENSO irregularity and predictability. This has implications for ENSO representation in low-resolution coupled models. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词El Niño–Southern Oscillation; Hybrid coupled model; Ocean general circulation model; Predictability; Stochastic forcing; Tropical instability waves
语种英语
scopus关键词El Nino-Southern Oscillation; instability; numerical model; oceanic general circulation model; prediction; stochasticity; tropical cyclone; Pacific Ocean; Pacific Ocean (Equatorial)
来源期刊Climate Dynamics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/146511
作者单位Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, Universityof New South Wales, Sydney, Australia; School of Mathematics and Statistics, University of New South Wales, Sydney, Australia; School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia; Centre for Southern Hemisphere Oceans Research (CSHOR), CSIRO Oceans and Atmosphere, Hobart, Australia
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Holmes R.M.,McGregor S.,Santoso A.,et al. Contribution of tropical instability waves to ENSO irregularity[J],2019,52(2020-03-04).
APA Holmes R.M.,McGregor S.,Santoso A.,&England M.H..(2019).Contribution of tropical instability waves to ENSO irregularity.Climate Dynamics,52(2020-03-04).
MLA Holmes R.M.,et al."Contribution of tropical instability waves to ENSO irregularity".Climate Dynamics 52.2020-03-04(2019).
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