Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1175/MWR-D-19-0342.1 |
Potential Vorticity Generation by West African Squall Lines | |
Johnson, Richard H.; Ciesielski, Paul E. | |
通讯作者 | Johnson, RH |
来源期刊 | MONTHLY WEATHER REVIEW
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ISSN | 0027-0644 |
EISSN | 1520-0493 |
出版年 | 2020 |
卷号 | 148期号:4页码:1691-1715 |
英文摘要 | The West African summer monsoon features multiple, complex interactions between African easterly waves (AEWs), moist convection, variable land surface properties, dust aerosols, and the diurnal cycle. One aspect of these interactions, the coupling between convection and AEWs, is explored using observations obtained during the 2006 African Monsoon Multidisciplinary Analyses (AMMA) field campaign. During AMMA, a research weather radar operated at Niamey, Niger, where it surveilled 28 squall-line systems characterized by leading convective lines and trailing stratiform regions. Nieto Ferreira et al. found that the squall lines were linked with the passage of AEWs and classified them into two tracks, northerly and southerly, based on the position of the African easterly jet (AEJ). Using AMMA sounding data, we create a composite of northerly squall lines that tracked on the cyclonic shear side of the AEJ. Latent heating within the trailing stratiform regions produced a midtropospheric positive potential vorticity (PV) anomaly centered at the melting level, as commonly observed in such systems. However, a unique aspect of these PV anomalies is that they combined with a 400-500-hPa positive PV anomaly extending southward from the Sahara. The latter feature is a consequence of the deep convective boundary layer over the hot Saharan Desert. Results provide evidence of a coupling and merging of two PV sources-one associated with the Saharan heat low and another with latent heating-that ends up creating a prominent midtropospheric positive PV maximum to the rear of West African squall lines. |
类型 | Article |
语种 | 英语 |
开放获取类型 | Bronze |
收录类别 | SCI-E |
WOS记录号 | WOS:000591341900013 |
WOS关键词 | ATMOSPHERIC BOUNDARY-LAYER ; TROPICAL CLOUD CLUSTERS ; SAHARAN AIR LAYER ; 23 JUNE 1981 ; EASTERLY WAVES ; THERMODYNAMIC STRUCTURE ; WEATHER SYSTEMS ; BUDGET ANALYSES ; SUMMER MONSOON ; DIURNAL CYCLE |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | Colorado State University |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/327585 |
作者单位 | [Johnson, Richard H.; Ciesielski, Paul E.] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA |
推荐引用方式 GB/T 7714 | Johnson, Richard H.,Ciesielski, Paul E.. Potential Vorticity Generation by West African Squall Lines[J]. Colorado State University,2020,148(4):1691-1715. |
APA | Johnson, Richard H.,&Ciesielski, Paul E..(2020).Potential Vorticity Generation by West African Squall Lines.MONTHLY WEATHER REVIEW,148(4),1691-1715. |
MLA | Johnson, Richard H.,et al."Potential Vorticity Generation by West African Squall Lines".MONTHLY WEATHER REVIEW 148.4(2020):1691-1715. |
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