The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis

Autor(es)

Drumond, A. ^[1] ; Marengo, J. ^[2] ; Ambrizzi, T. ^[3] ; Nieto, R. ^[1] ; Moreira, L. ^[4] ; Gimeno, L. ^[1]

Afiliação do(s) autor(es)

^[1] UVIGO, Fac Ciencias, Ephyslab, Orense - Spain

^[2] CCST INPE, Sao Paulo - Brazil

^[3] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, BR-09500900 Sao Paulo - Brazil

^[4] Univ Bern, Inst Appl Phys, CH-3012 Bern - Switzerland

• Tipo de documento: Artigo Científico
• Fonte: HYDROLOGY AND EARTH SYSTEM SCIENCES; v. 18, n. 7, p. 2577-2598, 2014.
• Citações Web of Science: 37

Resumo

We used a Lagrangian model (FLEXPART) together with the 1979-2012 ERA-Interim reanalysis data to investigate the role of the moisture in the Amazon Basin in the regional hydrological budget over the course of the year. FLEXPART computes budgets of evaporation minus precipitation by calculating changes in the specific humidity along forward and backward trajectories. The tropical Atlantic is the most important remote moisture source for the Amazon Basin. The tropical North Atlantic (NA) mainly contributed during the austral summer, while the contribution of the tropical South Atlantic (SA) prevailed for the remainder of the year. At the same time, the moisture contribution from the Amazon Basin itself is mainly for moisture supplying the southeastern South America. The 33-year temporal domain allowed the investigation of some aspects of the interannual variability of the moisture transport over the basin, such as the role of the El Nino Southern Oscillation (ENSO) and the Atlantic Meridional Mode (AMM) on the hydrological budget. During the peak of the Amazonian rainy season (from February to May, FMAM) the AMM is associated more with the interannual variations in the contribution from the tropical Atlantic sources, while the transport from the basin towards the subtropics responds more to the ENSO variability. The moisture contribution prevailed from the SA (NA) region in the years dominated by El Nino/positive AMM (La Nina/negative AMM) conditions. The transport from the Amazon towards the subtropics increased (reduced) during El Nino (La Nina) years. (AU)

• Processo FAPESP: 08/57719-9 - Programa de Mudanças Climáticas - INCT CLIMA
• Beneficiário: Carlos Afonso Nobre
• Linha de fomento: Auxílio à Pesquisa - Programa de Pesquisa sobre Mudanças Climáticas Globais - Temático
• Processo FAPESP: 08/58101-9 - Impact of the Southwestern Atlantic Ocean on South American climate for the 20th and 21st centuries
• Beneficiário: Tercio Ambrizzi
• Linha de fomento: Auxílio à Pesquisa - Programa de Pesquisa sobre Mudanças Climáticas Globais - Temático
• Processo FAPESP: 08/58161-1 - Assessment of impacts and vulnerability to climate change in Brazil and strategies for adaptation option
• Beneficiário: Jose Antonio Marengo Orsini
• Linha de fomento: Auxílio à Pesquisa - Programa de Pesquisa sobre Mudanças Climáticas Globais - Temático
• Processo FAPESP: 13/50538-7 - Entendimento das causas dos vieses que determinam o início da estação chuvosa na Amazônia nos modelos climáticos usando observações do GoAmazon e CHUVA
• Beneficiário: Jose Antonio Marengo Orsini
• Linha de fomento: Auxílio à Pesquisa - Regular