Behavior of the ITCZ second band near the Peruvian coast during the 2017 coastal El Niño

Descripción del Articulo

The behavior of the second band of the Intertropical Convergence Zone (ITCZ) near the Peruvian coast during early 2017 is studied, using precipitation, surface winds, sea surface temperature (SST) and atmospheric variables in different isobaric levels. The proposal of a daily index (Ia) to identify...

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Detalles Bibliográficos
Autores: Aliaga Nestares, Vannia, Rodríguez Zimmermann, Diego, Quispe, Nelson
Formato: artículo
Fecha de Publicación:2023
Institución:Servicio Nacional de Meteorología e Hidrología del Perú
Repositorio:SENAMHI-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.senamhi.gob.pe:20.500.12542/2565
Enlace del recurso:https://hdl.handle.net/20.500.12542/2565
Nivel de acceso:acceso abierto
Materia:Zonas Costeras
Atmospheric Circulation
Surface Wind
Lorenz Energy
ENSO
https://purl.org/pe-repo/ocde/ford#1.05.09
fenomeno El Niño - Clima y Eventos Naturales
Descripción
Sumario:The behavior of the second band of the Intertropical Convergence Zone (ITCZ) near the Peruvian coast during early 2017 is studied, using precipitation, surface winds, sea surface temperature (SST) and atmospheric variables in different isobaric levels. The proposal of a daily index (Ia) to identify opportunely the formation of this band and the Lorenz energy terms in the region is also considered. This band was present from late January to early April 2017, associated with an anomalous dipole of sea level pressure between the east and west eastern Equatorial Pacific that configured anomalously northerly surface winds and the release of southeasterly trade winds near Peru. In medium levels, a zonally oriented positive mixing ratio anomaly was observed in early March over the ITCZ second band, associated with heavy rain systems over the northern Peruvian coastal region. In the same period, positive anomalies of divergence in high tropospheric levels were observed. The daily Ia index allowed an effective detection of the ITCZ second band 11 days before the maximum coastal precipitation, and the Lorenz energy terms showed eddy kinetic energy (KE) peaks in January and February and a contribution of barotropic instability in equatorial regions.
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