Knowledge Management System Of Institute of Earth Environment, CAS
Towards understanding the suppressed ENSO activity during mid-Holocene in PMIP2 and PMIP3 simulations | |
Chen, Lin1,2,3; Zheng, Weipeng2,4; Braconnot, Pascale5 | |
通讯作者 | Chen, Lin(chenlin@nuist.edu.cn) ; Zheng, Weipeng(zhengwp@mail.iap.ac.cn) |
2019-07-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
卷号 | 53期号:1-2页码:1095-1110 |
摘要 | The mechanisms of El Nino-Southern Oscillation (ENSO) variability change during the mid-Holocene (MH) were investigated through analyzing the model simulations from the Paleoclimate Modelling Intercomparison Project Phases (PMIP) phase-2 and phase-3. The majority of PMIP2 and PMIP3 model simulations show a lower level of ENSO activity in the MH simulation compared to the pre-industrial (PI) simulation, which is qualitatively consistent with that inferred from the paleoclimate proxies. Through employing the Bjerknes stability index, we quantified the dynamic and thermodynamic air-sea feedbacks in the PI and MH simulations. The quantitative analyses showed that the reduced ENSO variability in MH arose from the weakening in the thermocline (TH), zonal-advection (ZA) and Ekman (EK) feedback terms. We found that all the weakened TH, ZA, and EK terms are associated with the reduction in the response of anomalous thermocline depth (D') to the zonal wind stress anomaly (x) in MH compared to PI. The reduced D' response is attributed to the flattened meridional structure of ENSO-related x field in MH, which is linked to the enhanced surface poleward mean meridional current in MH. Among many aspects of the mean state changes under the MH orbital forcing, this study identified that the surface mean meridional current change might be a key factor behind the suppressed ENSO variability in MH. Lastly, through comparing our findings with the ENSO future projection studies, we found that the wind-thermocline feedback is susceptible in a changing climate, which implies that minimizing the uncertainty in the wind-thermocline feedback change may help constrain future ENSO response. |
关键词 | ENSO amplitude change in mid-Holocene BJ index Air-sea feedback Ocean dynamical processes Meridional structure change |
DOI | 10.1007/s00382-019-04637-z |
关键词[WOS] | EL-NINO/SOUTHERN OSCILLATION ; TROPICAL PACIFIC CLIMATE ; LAST GLACIAL MAXIMUM ; SOUTHERN-OSCILLATION ; COUPLED SIMULATIONS ; NINO ; VARIABILITY ; MODEL ; OCEAN ; STABILITY |
收录类别 | SCI ; SCI |
语种 | 英语 |
资助项目 | National Key Research and Development Program on Monitoring, Early Warning and Prevention of Major Natural Disaster[2018YFC1506002] ; National Natural Science Foundation of China[41376002] ; National Natural Science Foundation of China[41705059] ; National Natural Science Foundation of China[41630423] ; National Natural Science Foundation of China[41606011] ; Startup Foundation for Introducing Talent of NUIST ; LASG Open Project ; open fund of State Key Laboratory of Loess and Quartary Geology[SKLLQG1802] ; National 973 project[2015CB453200] ; JPI Belmont project PACM-EDY[ANR-15-JCLI-0003-01] |
WOS研究方向 | Meteorology & Atmospheric Sciences |
项目资助者 | National Key Research and Development Program on Monitoring, Early Warning and Prevention of Major Natural Disaster ; National Natural Science Foundation of China ; Startup Foundation for Introducing Talent of NUIST ; LASG Open Project ; open fund of State Key Laboratory of Loess and Quartary Geology ; National 973 project ; JPI Belmont project PACM-EDY |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000471722400063 |
出版者 | SPRINGER |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ieecas.cn/handle/361006/13785 |
专题 | 黄土与第四纪地质国家重点实验室(2010~) |
通讯作者 | Chen, Lin; Zheng, Weipeng |
作者单位 | 1.Nanjing Univ Informat Sci & Technol, CIC FEMD, Joint Int Res Lab Climate & Environm Change ILCEC, Key Lab Meteorol Disaster,Minist Educ KLME, Nanjing 210044, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, SKLLQG, Xian 710061, Shaanxi, Peoples R China 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 5.Univ Paris Saclay, UVSQ, CNRS, LSCE,IPSL,CEA, Bat 714, F-91191 Gif Sur Yvette, France |
推荐引用方式 GB/T 7714 | Chen, Lin,Zheng, Weipeng,Braconnot, Pascale. Towards understanding the suppressed ENSO activity during mid-Holocene in PMIP2 and PMIP3 simulations[J]. CLIMATE DYNAMICS,2019,53(1-2):1095-1110. |
APA | Chen, Lin,Zheng, Weipeng,&Braconnot, Pascale.(2019).Towards understanding the suppressed ENSO activity during mid-Holocene in PMIP2 and PMIP3 simulations.CLIMATE DYNAMICS,53(1-2),1095-1110. |
MLA | Chen, Lin,et al."Towards understanding the suppressed ENSO activity during mid-Holocene in PMIP2 and PMIP3 simulations".CLIMATE DYNAMICS 53.1-2(2019):1095-1110. |
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