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Artículo

On the behavior of rainfall maxima at the eastern Andes

Hierro, Rodrigo FedericoIcon ; Burgos Fonseca, YuditsabetIcon ; Ramezani Ziarani, M.; Llamedo Soria, Pablo MartinIcon ; Schmidt, T.; de la Torre, AlejandroIcon ; Alexander, Pedro ManfredoIcon
Fecha de publicación: 04/2020
Editorial: Elsevier
Revista: Atmospheric Research
ISSN: 0169-8095
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:
Meteorología y Ciencias Atmosféricas

Resumen

In this study, we detect high percentile rainfall events in the eastern central Andes, based on Tropical Rainfall Measuring Mission (TRMM) with a spatial resolution of 0.25 × 0.25°, a temporal resolution of 3 h, and for the duration from 2001 to 2018. We identify three areas with high mean accumulated rainfall and analyze their atmospheric behaviour and rainfall characteristics with specific focus on extreme events. Extreme events are defined by events above the 95th percentile of their daily mean accumulated rainfall. Austral summer (DJF) is the period of the year presenting the most frequent extreme events over these three regions. Daily statistics show that the spatial maxima, as well as their associated extreme events, are produced during the night. For the considered period, ERA-Interim reanalysis data, provided by the European Centre for Medium-Range Weather Forecasts (ECMWF) with 0.75° x0.75° spatial and 6-hourly temporal resolutions, were used for the analysis of the meso- and synoptic-scale atmospheric patterns. Night- and day-time differences indicate a nocturnal overload of northerly and northeasterly low-level humidity flows arriving from tropical South America. Under these conditions, cooling descending air from the mountains may find unstable air at the surface, giving place to the development of strong local convection. Another possible mechanism is presented here: a forced ascent of the low-level flow due to the mountains, disrupting the atmospheric stratification and generating vertical displacement of air trajectories. A Principal Component Analysis (PCA) in T-mode is applied to day- and night-time data during the maximum and extreme events. The results show strong correlation areas over each subregion under study during night-time, whereas during day-time no defined patterns are found. This confirms the observed nocturnal behavior of rainfall within these three hotspots.
Palabras clave: PRECIPITATION , EXTREME EVENTS , ANDES
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info:eu-repo/semantics/openAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Atribución-NoComercial-SinDerivadas 2.5 Argentina (CC BY-NC-ND 2.5 AR)
Identificadores
URI: http://hdl.handle.net/11336/168444
URL: https://www.sciencedirect.com/science/article/pii/S0169809519310233
DOI: http://dx.doi.org/10.1016/j.atmosres.2019.104792
Colecciones
Articulos(SEDE CENTRAL)
Articulos de SEDE CENTRAL
Citación
Hierro, Rodrigo Federico; Burgos Fonseca, Yuditsabet; Ramezani Ziarani, M.; Llamedo Soria, Pablo Martin; Schmidt, T.; et al.; On the behavior of rainfall maxima at the eastern Andes; Elsevier; Atmospheric Research; 234; 4-2020; 1-26
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