中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Impacts of the Madden-Julian Oscillation on Marginal Sea Heatwaves of the Southeastern Tropical Indian Ocean

文献类型:期刊论文

作者Cui, Zhanxian1,3; Li, Yuanlong1,2,3; Guo, Yaru1; Wang, Fan1,2,3
刊名JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
出版日期2024-07-01
卷号129期号:7页码:19
关键词Madden-Julian Oscillation marine heatwaves intraseasonal temperature variability southeast tropical Indian Ocean
ISSN号2169-9275
DOI10.1029/2023JC020867
通讯作者Li, Yuanlong(liyuanlong@qdio.ac.cn)
英文摘要Marginal seas of the southeastern tropical Indian Ocean (SETIO), including the South Java coasts and the Timor and Arafura Seas, are hotspots of large-scale marine heatwaves (MHWs) in austral summer with notable impacts on local ecosystems. Yet, the prediction of these MHWs remains challenging. By analyzing 39 MHWs and 45 marine cold-spells (MCSs) observed in the summers of 1982-2021, this study reveals a robust modulation effect of the Madden-Julian Oscillation (MJO) on these events. The results show that 56% of MHWs and 51% of MCSs overlapped with MJO events, and their duration is systematically longer than others. Moreover, MHWs in phases 3-4 and MCSs in phases 6-7 of the real-time multivariate MJO (RMM) index were nearly 2-3 times stronger in intensity than the others. The passage of MJOs drives prominent intraseasonal sea surface temperature (SST) variability in the SETIO through perturbing surface heat fluxes, which in turn modulates the occurrence of MHWs and MCSs. During RMM phases 1-2 (convective center over of the east of Africa or the central-western Indian Ocean), the SETIO is controlled by a dry condition, with increased surface insolation and suppressed latent heat release. These anomalous fluxes drive a persistent SST increase, facilitating the emergence of strong and prolonged MHWs in the subsequent RMM phases 3-4. Further analysis suggests an 18% probability for MHWs in the SETIO 12 +/- 10 days after Phase 1. Therefore, the MJO contributes to the predictability of MHWs/MCSs of the SETIO, with implications for predicting climate extremes and hazards. The South Java coasts and the Timor and Arafura Seas in the southeastern tropical Indian Ocean (SETIO) suffer from frequent and strong marine heatwaves (MHWs) in austral summer. These events have significant impacts on the local environment. This research explores how the Madden-Julian Oscillation (MJO) affects these MHWs and marine cold-spells (MCSs). We find that MHWs and MCSs occurring with MJOs tend to persist longer than others. MHWs are overall stronger in phases 3-4 of the real-time multivariate MJO (RMM) index than the others, while MCSs are enhanced in RMM phases 6-7. The MJO causes sea surface temperature (SST) variability in the SETIO through surface heat fluxes. In RMM phases 1-2, the SETIO experiences dry condition with increased solar radiation and reduced wind speed, enhancing the likelihood of strong MHWs in subsequent phases 3-4. MJO is potentially helpful in predicting MHWs and MCSs. For example, there is an 18% probability of the MHW in the SETIO when the MJO evolves to RMM Phase 3 from RMM Phase 1 within 12 +/- 10 days. This probability exceeds the 95% background occurrence probability (similar to 4%) by four folds. Generally, eastward propagating MJOs contribute to the predictability of MHWs/MCSs in the SETIO. Marine heatwaves (MHWs) in the southeastern tropical Indian Ocean (SETIO) are modulated by MJOs and significantly enhanced in real-time multivariate MJO phases 3-4 MJOs drive intraseasonal temperature variability in the SETIO by surface shortwave radiation and latent heat flux and thereby modulate MHWs The eastward-propagating MJOs effectively contribute to the predictability of MHWs and marine cold-spells in the SETIO
WOS关键词MARINE HEAT-WAVE ; INTRASEASONAL VARIABILITY ; INDONESIAN THROUGHFLOW ; WESTERN-AUSTRALIA ; SUMMER ; MJO ; SST ; PREDICTABILITY ; PACIFIC ; INCREASE
资助项目Strategic Priority Research Program of Chinese Academy of Sciences[XDB42000000] ; Natural Science Foundation of China[42090044] ; Laoshan Laboratory[LSKJ202202601] ; Ocean Science Data Center, IOCAS
WOS研究方向Oceanography
语种英语
WOS记录号WOS:001262811100001
出版者AMER GEOPHYSICAL UNION
源URL[http://ir.qdio.ac.cn/handle/337002/186299]  
专题海洋研究所_海洋环流与波动重点实验室
通讯作者Li, Yuanlong
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
2.Laoshan Lab, Qingdao, Peoples R China
3.Univ Chinese Acad Sci, Beijing, Peoples R China
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Cui, Zhanxian,Li, Yuanlong,Guo, Yaru,et al. Impacts of the Madden-Julian Oscillation on Marginal Sea Heatwaves of the Southeastern Tropical Indian Ocean[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2024,129(7):19.
APA Cui, Zhanxian,Li, Yuanlong,Guo, Yaru,&Wang, Fan.(2024).Impacts of the Madden-Julian Oscillation on Marginal Sea Heatwaves of the Southeastern Tropical Indian Ocean.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,129(7),19.
MLA Cui, Zhanxian,et al."Impacts of the Madden-Julian Oscillation on Marginal Sea Heatwaves of the Southeastern Tropical Indian Ocean".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 129.7(2024):19.

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来源:海洋研究所

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