Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia
The impact of the Atlantic Multidecadal Oscillation (AMO) on the variations in the streamflow in the Atrato River Basin (ARB) during the 1965−2016 period was analyzed here by considering the cold (1965−1994) and warm (1995−2015) phases of this oscillation. The mean stre...
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doaj-fcab1438dd254e92accde0305c2e3f042020-11-25T02:13:03ZengMDPI AGWater2073-44412020-01-0112121610.3390/w12010216w12010216Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern ColombiaWilmar Loaiza Cerón0Mary Toshie Kayano1Rita Valeria Andreoli2Alvaro Avila3Teresita Canchala4Félix Francés5Irma Ayes Rivera6Wilfredo Alfonso-Morales7Rodrigo Augusto Ferreira de Souza8Yesid Carvajal-Escobar9Department of Geography, Faculty of Humanities, Universidad del Valle, Calle 13 #100-00, Cali 25360, ColombiaInstituto Nacional de Pesquisas Espaciais, Centro de Previsão de Tempo e Estudos Climáticos, Divisão de Modelagem e Desenvolvimento. Av. dos Astronautas 1758, São José dos Campos 12227-010, BrazilEscola Superior de Tecnologia, Universidade do Estado do Amazonas, Av. Darcy Vargas 1200, Parque 10 de Novembro, Manaus 69065-020, BrazilDepartment of Agricultural Engineering, Federal University of Viçosa, Viçosa 36570-900, BrazilResearch Group in Water Resources Engineering and Soil (IREHISA), School of natural Resources and Environmental Engineering, Universidad del Valle, Calle 13 #100-00, Cali 25360, ColombiaResearch Group of Hydrological and Environmental Modelling (GIMHA), Research Institute of Water and Environmental Engineering (IIAMA), Universitat Politècnica de València, 46022 Valencia, SpainPostgraduation Program CLIAMB, Instituto Nacional de Pesquisas da Amazônia (INPA)—Universidade do Estado do Amazonas (UEA), Ave. André Araújo 2936, Manaus 69060-001, BrazilResearch Group of Perception and Intelligent Systems (PSI), School of Electrical and Electronic Engineering, Universidad del Valle, Calle 13 #100-00, Cali 25360, ColombiaEscola Superior de Tecnologia, Universidade do Estado do Amazonas, Av. Darcy Vargas 1200, Parque 10 de Novembro, Manaus 69065-020, BrazilEngineering School, Natural and Environmental Resources Engineering School (EIDENAR), Universidad del Valle, Calle 13 #100-00, Cali 25360, ColombiaThe impact of the Atlantic Multidecadal Oscillation (AMO) on the variations in the streamflow in the Atrato River Basin (ARB) during the 1965−2016 period was analyzed here by considering the cold (1965−1994) and warm (1995−2015) phases of this oscillation. The mean streamflow increased after 1994 (AMO phase change). This increase is related to the strengthening of the zonal gradients of the sea surface temperature (SST) and sea level pressure (SLP) between the tropical central Pacific and the tropical Atlantic after 1994 (warm AMO phase). These gradients contributed to strengthen the Walker cell related upward movement over northern and northwestern South America, in particular during November-December (ND). Consistently, the frequency (R20 mm) and intensity (SDII) of extreme daily rainfall events increased during the 1995−2015 period. Our results show a connection between the AMO and the increase in the streamflow in the ARB during the last five decades. These results contribute to the studies of resilience and climate adaptation in the region.https://www.mdpi.com/2073-4441/12/1/216atlantic multidecadal oscillationclimate variabilitystreamflowrainfallatrato river basin |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Wilmar Loaiza Cerón Mary Toshie Kayano Rita Valeria Andreoli Alvaro Avila Teresita Canchala Félix Francés Irma Ayes Rivera Wilfredo Alfonso-Morales Rodrigo Augusto Ferreira de Souza Yesid Carvajal-Escobar |
spellingShingle |
Wilmar Loaiza Cerón Mary Toshie Kayano Rita Valeria Andreoli Alvaro Avila Teresita Canchala Félix Francés Irma Ayes Rivera Wilfredo Alfonso-Morales Rodrigo Augusto Ferreira de Souza Yesid Carvajal-Escobar Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia Water atlantic multidecadal oscillation climate variability streamflow rainfall atrato river basin |
author_facet |
Wilmar Loaiza Cerón Mary Toshie Kayano Rita Valeria Andreoli Alvaro Avila Teresita Canchala Félix Francés Irma Ayes Rivera Wilfredo Alfonso-Morales Rodrigo Augusto Ferreira de Souza Yesid Carvajal-Escobar |
author_sort |
Wilmar Loaiza Cerón |
title |
Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia |
title_short |
Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia |
title_full |
Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia |
title_fullStr |
Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia |
title_full_unstemmed |
Streamflow Intensification Driven by the Atlantic Multidecadal Oscillation (AMO) in the Atrato River Basin, Northwestern Colombia |
title_sort |
streamflow intensification driven by the atlantic multidecadal oscillation (amo) in the atrato river basin, northwestern colombia |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2020-01-01 |
description |
The impact of the Atlantic Multidecadal Oscillation (AMO) on the variations in the streamflow in the Atrato River Basin (ARB) during the 1965−2016 period was analyzed here by considering the cold (1965−1994) and warm (1995−2015) phases of this oscillation. The mean streamflow increased after 1994 (AMO phase change). This increase is related to the strengthening of the zonal gradients of the sea surface temperature (SST) and sea level pressure (SLP) between the tropical central Pacific and the tropical Atlantic after 1994 (warm AMO phase). These gradients contributed to strengthen the Walker cell related upward movement over northern and northwestern South America, in particular during November-December (ND). Consistently, the frequency (R20 mm) and intensity (SDII) of extreme daily rainfall events increased during the 1995−2015 period. Our results show a connection between the AMO and the increase in the streamflow in the ARB during the last five decades. These results contribute to the studies of resilience and climate adaptation in the region. |
topic |
atlantic multidecadal oscillation climate variability streamflow rainfall atrato river basin |
url |
https://www.mdpi.com/2073-4441/12/1/216 |
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