Influence of Tropical Easterly Waves on the ChocoJet during the 2019 OTREC Campaign

被引:1
|
作者
Valencia, Juliana [1 ]
Yepes, Johanna [1 ]
Mejia, John F. [2 ]
Builes-Jaramillo, Lejandro [1 ]
Salas, Hernan D. [1 ,3 ]
机构
[1] Inst Univ Colegio Mayor Antioquia, Fac Arquitectura Ingn, Medellin, Colombia
[2] Desert Res Inst, Dept Atmospher Sci, Reno, NV 89512 USA
[3] Inst Tecnol Metropolitano, Fac Ciencias Exactas & Aplicadas, Medellin, Colombia
关键词
Atmospheric waves; Jets; Synoptic-scale processes; Tropical cyclones; Hydrometeorology; Field experiments; AMERICA; CONVECTION; PRECIPITATION; CLIMATOLOGY; VARIABILITY; CIRCULATION; ATMOSPHERE; SUMMER;
D O I
10.1175/JHM-D-23-0039.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study investigates how convectively coupled tropical easterly waves (TEWs) affect the Choco low-level jet (ChocoJet) as they move across the western Caribbean. The ChocoJet is a low-level flow over the eastern Pacific (EPAC) that modulates precipitation patterns over the tropical eastern Pacific and northwestern South America. By comysis products, and satellite data, we analyze precipitation and circulation patterns during convectively coupled and nonconvectively coupled TEWs, comparing them to non-TEW days. During convectively coupled TEWs days, the ChocoJet strengthens and becomes more southerly, while the ITCZ moves northward, leading to enhanced precipitation over the western Caribbean and drier conditions over the northern part of the Colombian Pacific. In contrast, nonconvectively coupled TEW days exhibit reduced precipitation and precipitable water over the Caribbean and far EPAC, with a layer of northeasterly flow centered at 850 hPa flowing over a shallower, weaker, and more westerly ChocoJet. Additionally, convectively coupled TEWs are associated with a weaker western Caribbean and far eastern Pacific pressure gradient compared to nonconvective TEWs. These observable and predictable synoptic-scale circulation-precipitation relationships contribute to a better understanding of hydrometeorological variability in the region.
引用
收藏
页码:325 / 337
页数:13
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