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DOI | 10.1007/s00382-016-3270-9 |
ENSO feedbacks and their relationships with the mean state in a flux adjusted ensemble | |
Ferrett S.; Collins M. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 7189 |
结束页码 | 7208 |
卷号 | 52期号:12 |
英文摘要 | The El Niño Southern Oscillation (ENSO) is governed by a combination of amplifying and damping ocean–atmosphere feedbacks in the equatorial Pacific. Here we quantify these feedbacks in a flux adjusted HadCM3 perturbed physics ensemble under present day conditions and a future emissions scenario using the Bjerknes Stability Index (BJ index). Relationships between feedbacks and both the present day biases and responses under climate change of the mean equatorial Pacific climate are investigated. Despite minimised mean sea surface temperature biases through flux adjustment, the important dominant ENSO feedbacks still show biases with respect to observed feedbacks and inter-ensemble diversity. The dominant positive thermocline and zonal advective feedbacks are found to be weaker in ensemble members with stronger mean zonal advection. This is due to a weaker sensitivity of the thermocline slope and zonal surface ocean currents in the east Pacific to surface wind stress anomalies. A drier west Pacific is also found to be linked to weakened shortwave and latent heat flux damping, suggesting a link between ENSO characteristics and the hydrological cycle. In contrast to previous studies using the BJ index that find positive relationships between the index and ENSO amplitude, here they are weakly or negatively correlated, both for present day conditions and for projected differences. This is caused by strong thermodynamic damping which dominates over positive feedbacks, which alone approximate ENSO amplitude well. While the BJ index proves useful for individual linear feedback analysis, we urge caution in using the total linear BJ index alone to assess the reasons for ENSO amplitude biases and its future change in models. © 2016, The Author(s). |
英文关键词 | ENSO; Feedbacks; Pacific; Stability |
语种 | 英语 |
scopus关键词 | climate change; climate feedback; El Nino-Southern Oscillation; latent heat flux; sea surface temperature; wind stress; Pacific Ocean; Pacific Ocean (Equatorial); Pacific Ocean (West) |
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/146293 |
作者单位 | College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom |
推荐引用方式 GB/T 7714 | Ferrett S.,Collins M.. ENSO feedbacks and their relationships with the mean state in a flux adjusted ensemble[J],2019,52(12). |
APA | Ferrett S.,&Collins M..(2019).ENSO feedbacks and their relationships with the mean state in a flux adjusted ensemble.Climate Dynamics,52(12). |
MLA | Ferrett S.,et al."ENSO feedbacks and their relationships with the mean state in a flux adjusted ensemble".Climate Dynamics 52.12(2019). |
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