Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin

Mesoscale convective systems (MCSs) climatology, the thermodynamic and dynamical variables, and teleconnections influencing MCSs development are assessed for the Paute basin (PB) in the Ecuadorian Andes from 2000 to 2009. The seasonality of MCSs occurrence shows a bimodal pattern, with higher occurr...

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Main Authors: Lenin Campozano, Katja Trachte, Rolando Célleri, Esteban Samaniego, Joerg Bendix, Cristóbal Albuja, John F. Mejia
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/4259191
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author Lenin Campozano
Katja Trachte
Rolando Célleri
Esteban Samaniego
Joerg Bendix
Cristóbal Albuja
John F. Mejia
author_facet Lenin Campozano
Katja Trachte
Rolando Célleri
Esteban Samaniego
Joerg Bendix
Cristóbal Albuja
John F. Mejia
author_sort Lenin Campozano
collection DOAJ
description Mesoscale convective systems (MCSs) climatology, the thermodynamic and dynamical variables, and teleconnections influencing MCSs development are assessed for the Paute basin (PB) in the Ecuadorian Andes from 2000 to 2009. The seasonality of MCSs occurrence shows a bimodal pattern, with higher occurrence during March-April (MA) and October-November (ON), analogous to the regional rainfall seasonality. The diurnal cycle of MCSs shows a clear nocturnal occurrence, especially during the MA and ON periods. Interestingly, despite the higher occurrence of MCSs during the rainy seasons, the monthly size relative frequency remains fairly constant throughout the year. On the east of the PB, the persistent high convective available potential and low convective inhibition values from midday to nighttime are likely related to the nocturnal development of the MCSs. A significant positive correlation between the MCSs occurrence to the west of the PB and the Trans-Niño index was found, suggesting that ENSO is an important source of interannual variability of MCSs frequency with increasing development of MCSs during warm ENSO phases. On the east of the PB, the variability of MCSs is positively correlated to the tropical Atlantic sea surface temperature anomalies south of the equator, due to the variability of the Atlantic subtropical anticyclone, showing main departures from this relation when anomalous conditions occur in the tropical Pacific due to ENSO.
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spelling doaj-art-a3b0c233a9354e8a82d4fdd6efa1e12e2025-02-03T01:02:02ZengWileyAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/42591914259191Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute BasinLenin Campozano0Katja Trachte1Rolando Célleri2Esteban Samaniego3Joerg Bendix4Cristóbal Albuja5John F. Mejia6Departamento de Recursos Hídricos y Ciencias Ambientales, Universidad de Cuenca, Cuenca, EcuadorLaboratory for Climatology and Remote Sensing (LCRS), Faculty of Geography, Philipps-University Marburg, Deutschhausstraße 10, 35032 Marburg, GermanyDepartamento de Recursos Hídricos y Ciencias Ambientales, Universidad de Cuenca, Cuenca, EcuadorDepartamento de Recursos Hídricos y Ciencias Ambientales, Universidad de Cuenca, Cuenca, EcuadorLaboratory for Climatology and Remote Sensing (LCRS), Faculty of Geography, Philipps-University Marburg, Deutschhausstraße 10, 35032 Marburg, GermanyDepartamento de Recursos Hídricos y Ciencias Ambientales, Universidad de Cuenca, Cuenca, EcuadorDepartment of Atmospheric Sciences, Desert Research Institute, Reno, NV, USAMesoscale convective systems (MCSs) climatology, the thermodynamic and dynamical variables, and teleconnections influencing MCSs development are assessed for the Paute basin (PB) in the Ecuadorian Andes from 2000 to 2009. The seasonality of MCSs occurrence shows a bimodal pattern, with higher occurrence during March-April (MA) and October-November (ON), analogous to the regional rainfall seasonality. The diurnal cycle of MCSs shows a clear nocturnal occurrence, especially during the MA and ON periods. Interestingly, despite the higher occurrence of MCSs during the rainy seasons, the monthly size relative frequency remains fairly constant throughout the year. On the east of the PB, the persistent high convective available potential and low convective inhibition values from midday to nighttime are likely related to the nocturnal development of the MCSs. A significant positive correlation between the MCSs occurrence to the west of the PB and the Trans-Niño index was found, suggesting that ENSO is an important source of interannual variability of MCSs frequency with increasing development of MCSs during warm ENSO phases. On the east of the PB, the variability of MCSs is positively correlated to the tropical Atlantic sea surface temperature anomalies south of the equator, due to the variability of the Atlantic subtropical anticyclone, showing main departures from this relation when anomalous conditions occur in the tropical Pacific due to ENSO.http://dx.doi.org/10.1155/2018/4259191
spellingShingle Lenin Campozano
Katja Trachte
Rolando Célleri
Esteban Samaniego
Joerg Bendix
Cristóbal Albuja
John F. Mejia
Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
Advances in Meteorology
title Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
title_full Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
title_fullStr Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
title_full_unstemmed Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
title_short Climatology and Teleconnections of Mesoscale Convective Systems in an Andean Basin in Southern Ecuador: The Case of the Paute Basin
title_sort climatology and teleconnections of mesoscale convective systems in an andean basin in southern ecuador the case of the paute basin
url http://dx.doi.org/10.1155/2018/4259191
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