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DOI | 10.1007/s00382-019-05108-1 |
Remote influences on the Indian monsoon low-level jet intraseasonal variations | |
Swathi M.S.; Izumo T.; Lengaigne M.; Vialard J.; Kumar M.R.R. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 2221 |
结束页码 | 2236 |
卷号 | 54 |
英文摘要 | A strong low-level jet (LLJ), also known as the Findlater jet, develops over the Arabian Sea during the Indian summer monsoon. This jet is an essential source of moisture for monsoonal rainfall over the densely-populated Indian subcontinent and is a key contributor to the Indian Ocean oceanic productivity by sustaining the western Arabian Sea upwelling systems. The LLJ intensity fluctuates intraseasonally within the ~ 20- to 90-day band, in relation with the northward-propagating active and break phases of the Indian summer monsoon. Our observational analyses reveal that these large-scale regional convective perturbations only explain about half of the intraseasonal LLJ variance, the other half being unrelated to large-scale convective perturbations over the Indian Ocean. We show that convective fluctuations in two regions outside the Indian Ocean can remotely force a LLJ intensification, four days later. Enhanced atmospheric deep convection over the northwestern tropical Pacific yields westerly wind anomalies that propagate westward to the Arabian Sea as baroclinic atmospheric Rossby Waves. Suppressed convection over the eastern Pacific/North American monsoon region yields westerly wind anomalies that propagate eastward to the Indian Ocean as dry baroclinic equatorial Kelvin waves. Those largely independent remote influences jointly explain ~ 40% of the intraseasonal LLJ variance that is not related to convective perturbations over the Indian Ocean (i.e. ~ 20% of the total), with the northwestern Pacific contributing twice as much as the eastern Pacific. Taking into account these two remote influences should thus enhance the ability to predict the LLJ. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. |
语种 | 英语 |
scopus关键词 | air-sea interaction; atmospheric convection; jet flow; Kelvin wave; monsoon; perturbation; seasonal variation; upwelling; Arabian Sea; Indian Ocean |
来源期刊 | Climate Dynamics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145577 |
作者单位 | CSIR-National Institute of Oceanography, Goa, India; Sorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Paris, France; Indo-French Cell for Water Sciences, IISc-NIO-IITM–IRD Joint International Laboratory, NIO, Goa, India |
推荐引用方式 GB/T 7714 | Swathi M.S.,Izumo T.,Lengaigne M.,et al. Remote influences on the Indian monsoon low-level jet intraseasonal variations[J],2020,54. |
APA | Swathi M.S.,Izumo T.,Lengaigne M.,Vialard J.,&Kumar M.R.R..(2020).Remote influences on the Indian monsoon low-level jet intraseasonal variations.Climate Dynamics,54. |
MLA | Swathi M.S.,et al."Remote influences on the Indian monsoon low-level jet intraseasonal variations".Climate Dynamics 54(2020). |
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