Climate Change Data Portal
DOI | 10.1007/s00382-020-05401-4 |
A quasi-geostrophic diagnosis of the zonal flow associated with cut-off lows over South Africa and surrounding oceans | |
Ndarana T.; Rammopo T.S.; Chikoore H.; Barnes M.A.; Bopape M.-J. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 2631 |
结束页码 | 2644 |
卷号 | 55 |
英文摘要 | The zonal flow associated with cut-off lows (COLs) comprises two jet streaks of different spatial extents. The smaller scale jet streak, located north of the COLs, forms as a result of meridional divergence of vorticity advection and it is quasi-stationary, relative to the COLs. It dissipates as the COLs do the same. The larger scale jet streak gives rise to anticyclonic and equatorward Rossby wave breaking (RWB) as it propagates southeasterly to the base of the ridge, south of the COL and then northeasterly beyond that point. As the jet streak propagates it brings with it the anticyclonic barotropic shear that causes the Rossby waves to break. Its propagation is caused by zonal momentum advection by the zonal flow from jet streak entrance to its exit. As it propagates, its northwesterly/southeasterly orientation changes to one that is more zonal to become south-westerly/northeasterly at the end of the COL life cycle. This change in orientation is due to meridional advection of zonal momentum,where the meridional flow advects momentum southward (northward) at the jet streak entrance (exit). The jet streaks form a split jet structure and the winds between the streaks is decelerated by vorticity advection convergence. Because the flow and COL (and RWB) life cycle are coupled, understanding the dynamics that underlie the changes in the COL ambient flow contributes to resolving the outstanding RWB/COL causality problem. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Cut-off low; Geostrophic flow; Jet streak; Rossby wave breaking |
语种 | 英语 |
scopus关键词 | advection; anticyclone; barotropic motion; geostrophic flow; jet stream; meridional circulation; Rossby wave; vorticity; wave breaking; zonal flow; South Africa |
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/145277 |
作者单位 | Geography, Geoinformatics and Meteorology, University of Pretoria, Hatfield, South Africa; Unit for Environmental Sciences and Management, North-West University, Vanderbijlpark, South Africa; Marine Research Unit, South African Weather Service, Cape Town, South Africa; Department of Research and Innovation, South African Weather Service, Centurion, South Africa |
推荐引用方式 GB/T 7714 | Ndarana T.,Rammopo T.S.,Chikoore H.,et al. A quasi-geostrophic diagnosis of the zonal flow associated with cut-off lows over South Africa and surrounding oceans[J],2020,55. |
APA | Ndarana T.,Rammopo T.S.,Chikoore H.,Barnes M.A.,&Bopape M.-J..(2020).A quasi-geostrophic diagnosis of the zonal flow associated with cut-off lows over South Africa and surrounding oceans.Climate Dynamics,55. |
MLA | Ndarana T.,et al."A quasi-geostrophic diagnosis of the zonal flow associated with cut-off lows over South Africa and surrounding oceans".Climate Dynamics 55(2020). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。