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spelling paper:paper_00221694_v365_n1-2_p105_Panarello2023-06-08T14:46:52Z Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition Deuterium excess ENSO ITCZ Paraná River Stable isotopes Catchments Deuterium Hydrogen Isotopes Moisture Nickel compounds Oxygen All over the worlds Amazon rivers Buenos aires , argentina ENSO Evaporation processes Inter tropical convergence zones Isotope compositions ITCZ Meteorological phenomenons Periodic variations Positive correlations South america Stable isotopes Transit times Rivers El Nino-Southern Oscillation hydrochemistry hydrogen isotope intertropical convergence zone isotopic composition nitrogen isotope oxygen isotope stable isotope Parana River South America The Paraná River, the second in discharge in South America after the Amazon River and the fifth all over the world, releases an average of more than 17 000 m3 s-1 into the Del Plata Estuary. In order to assess the causes of variations in its stable isotope composition, 120 monthly grab samples of the Paraná River, acquired on a period of 10 years at the river mouth, near Ciudad Universitaria, Buenos Aires, Argentina have been analysed for oxygen and hydrogen stable isotopes. Both, 2H and 18O showed periodic variations (δ18O between -7‰ and -3‰; δ2H between -44‰ and -15‰) that follow, shifted in ca. 4 months (average transit time of the river), the southward excursions of the intertropical convergence zone (ITCZ). Deuterium excess values (δ2H - 8δ18O) also exhibited large variations (3-18‰) and showed a positive correlation with the El Niño South Oscillation Phenomenon (ENSO) index. ENSO affects the kinetic of the evaporation process of water and modifies the degree in which ITCZ shifts southwards capturing variable amounts of deuterium-rich recycled moisture from the Amazon's basin, then precipitating on the catchment's areas of the Paraná River. © 2008 Elsevier B.V. All rights reserved. 2009 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00221694_v365_n1-2_p105_Panarello http://hdl.handle.net/20.500.12110/paper_00221694_v365_n1-2_p105_Panarello
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Deuterium excess
ENSO
ITCZ
Paraná River
Stable isotopes
Catchments
Deuterium
Hydrogen
Isotopes
Moisture
Nickel compounds
Oxygen
All over the worlds
Amazon rivers
Buenos aires , argentina
ENSO
Evaporation processes
Inter tropical convergence zones
Isotope compositions
ITCZ
Meteorological phenomenons
Periodic variations
Positive correlations
South america
Stable isotopes
Transit times
Rivers
El Nino-Southern Oscillation
hydrochemistry
hydrogen isotope
intertropical convergence zone
isotopic composition
nitrogen isotope
oxygen isotope
stable isotope
Parana River
South America
spellingShingle Deuterium excess
ENSO
ITCZ
Paraná River
Stable isotopes
Catchments
Deuterium
Hydrogen
Isotopes
Moisture
Nickel compounds
Oxygen
All over the worlds
Amazon rivers
Buenos aires , argentina
ENSO
Evaporation processes
Inter tropical convergence zones
Isotope compositions
ITCZ
Meteorological phenomenons
Periodic variations
Positive correlations
South america
Stable isotopes
Transit times
Rivers
El Nino-Southern Oscillation
hydrochemistry
hydrogen isotope
intertropical convergence zone
isotopic composition
nitrogen isotope
oxygen isotope
stable isotope
Parana River
South America
Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
topic_facet Deuterium excess
ENSO
ITCZ
Paraná River
Stable isotopes
Catchments
Deuterium
Hydrogen
Isotopes
Moisture
Nickel compounds
Oxygen
All over the worlds
Amazon rivers
Buenos aires , argentina
ENSO
Evaporation processes
Inter tropical convergence zones
Isotope compositions
ITCZ
Meteorological phenomenons
Periodic variations
Positive correlations
South america
Stable isotopes
Transit times
Rivers
El Nino-Southern Oscillation
hydrochemistry
hydrogen isotope
intertropical convergence zone
isotopic composition
nitrogen isotope
oxygen isotope
stable isotope
Parana River
South America
description The Paraná River, the second in discharge in South America after the Amazon River and the fifth all over the world, releases an average of more than 17 000 m3 s-1 into the Del Plata Estuary. In order to assess the causes of variations in its stable isotope composition, 120 monthly grab samples of the Paraná River, acquired on a period of 10 years at the river mouth, near Ciudad Universitaria, Buenos Aires, Argentina have been analysed for oxygen and hydrogen stable isotopes. Both, 2H and 18O showed periodic variations (δ18O between -7‰ and -3‰; δ2H between -44‰ and -15‰) that follow, shifted in ca. 4 months (average transit time of the river), the southward excursions of the intertropical convergence zone (ITCZ). Deuterium excess values (δ2H - 8δ18O) also exhibited large variations (3-18‰) and showed a positive correlation with the El Niño South Oscillation Phenomenon (ENSO) index. ENSO affects the kinetic of the evaporation process of water and modifies the degree in which ITCZ shifts southwards capturing variable amounts of deuterium-rich recycled moisture from the Amazon's basin, then precipitating on the catchment's areas of the Paraná River. © 2008 Elsevier B.V. All rights reserved.
title Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
title_short Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
title_full Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
title_fullStr Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
title_full_unstemmed Large scale meteorological phenomena, ENSO and ITCZ, define the Paraná River isotope composition
title_sort large scale meteorological phenomena, enso and itcz, define the paraná river isotope composition
publishDate 2009
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00221694_v365_n1-2_p105_Panarello
http://hdl.handle.net/20.500.12110/paper_00221694_v365_n1-2_p105_Panarello
_version_ 1768543310860779520