Interhemispheric influence of Indo-Pacific convection oscillation on Southern Hemisphere rainfall through southward propagation of Rossby waves
文献类型:期刊论文
作者 | Zheng, Jiayu5; Zhao, Sen; Li, Jianping1,2,3; Li, Yanjie4; Jin, Fei-Fei |
刊名 | CLIMATE DYNAMICS
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出版日期 | 2019 |
卷号 | 52期号:2019-05-06页码:3203 |
关键词 | Interhemispheric teleconnection Indo-Pacific convection oscillation Rossby waves Boreal summer Cross-equatorial propagation Rainfall |
ISSN号 | 0930-7575 |
DOI | 10.1007/s00382-018-4324-y |
英文摘要 | Tropical Indo-western Pacific convection anomalies influence atmospheric circulation, impacting climate far beyond the tropics. Here we present observational and modelling evidence for an interhemispheric effect of the boreal summer (June-August) Indo-Pacific convection oscillation (IPCO), which is characterized by a zonal seesaw pattern between the north Indian Ocean (NIO) and the western North Pacific (WNP). It is found that the IPCO is significantly correlated with simultaneous rainfall over many parts of the Southern Hemisphere (SH), including western Australia and western Brazil. These interhemispheric connections in rainfall remain significant when then El Nino-Southern Oscillation, the Indian Ocean Dipole, and the SH Annular Mode related signals are excluded simultaneously, which may help to improve the SH seasonal predictions. The physical mechanism that underlies this interhemispheric connection is investigated using observations, Rossby wave diagnostics and a series of atmospheric model experiments. Results suggest that convective heating anomalies associated with the IPCO excite two distinct southward-propagating equivalent barotropic wave trains that propagate into the extratropics in the SH: the South Africa-mid-latitudes wave train excited by the heat sink over the NIO, and the Maritime Continent-subtropical Australia wave train excited by the heat source over the WNP. We further demonstrate that upper tropospheric northerlies over tropical Africa and the Indian Ocean are responsible for the southward propagation of stationary Rossby waves across the easterlies. These equivalent barotropic waves then modulate the moisture transport, baroclinicity, and mid-latitude storminess, and thus affect rainfall anomalies in the SH. The new wave train patterns provide novel insight into the teleconnection pathways of convective heating over the tropical Indian Ocean and western Pacific. |
源URL | [http://ir.scsio.ac.cn/handle/344004/17756] ![]() |
专题 | 南海海洋研究所_热带海洋环境国家重点实验室(LTO) |
作者单位 | 1.Univ Hawaii Manoa, Dept Atmospher Sci, Honolulu, HI 96822 USA 2.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China 3.Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao 266237, Shandong, Peoples R China 5.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China 6.Nanjing Univ Informat Sci & Technol, Coll Atmospher Sci, Minist Educ, CIC,FEMD,ILCEC,Key Lab Meteorol Disaster, Nanjing 210044, Jiangsu, Peoples R China 7.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China |
推荐引用方式 GB/T 7714 | Zheng, Jiayu,Zhao, Sen,Li, Jianping,et al. Interhemispheric influence of Indo-Pacific convection oscillation on Southern Hemisphere rainfall through southward propagation of Rossby waves[J]. CLIMATE DYNAMICS,2019,52(2019-05-06):3203, 3221. |
APA | Zheng, Jiayu,Zhao, Sen,Li, Jianping,Li, Yanjie,&Jin, Fei-Fei.(2019).Interhemispheric influence of Indo-Pacific convection oscillation on Southern Hemisphere rainfall through southward propagation of Rossby waves.CLIMATE DYNAMICS,52(2019-05-06),3203. |
MLA | Zheng, Jiayu,et al."Interhemispheric influence of Indo-Pacific convection oscillation on Southern Hemisphere rainfall through southward propagation of Rossby waves".CLIMATE DYNAMICS 52.2019-05-06(2019):3203. |
入库方式: OAI收割
来源:南海海洋研究所
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