Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo

Bibliographic Details
Main Author: Dos Santos, Vinícius [UNESP]
Publication Date: 2019
Other Authors: Gastmans, Didier [UNESP], Santarosa, Lucas Vituri [UNESP], Batista, Ludmila Vianna [UNESP], Betancur, Sebastian Balbin [UNESP], De Oliverira, Marcelo Eduardo Dias [UNESP], Filho, Augusto José Pereira
Format: Article
Language: por
Source: Repositório Institucional da UNESP
Download full: http://dx.doi.org/10.14295/ras.v33i2.29474
https://hdl.handle.net/11449/302299
Summary: Water stable isotopes have been used as a tool in hydrometeorological studies, generating relevant information about the relationship between climate and groundwater recharge as well as determining surface water flows origin, contributing to the understanding of the consequences of climate change on the hydrological cycle. The present work presents the main climatic controls responsible for the variability in the precipitation monthly isotopic composition in the central region of São Paulo state, where areas of recharge of important aquifers of the Paraná Basin are located. Local meteoric water line (δ2H = 8.34 * δ18O + 15.71) indicates that the isotopic composition is influenced by a source of oceanic moisture and vapor recirculation processes along the displacement of air masses over the continent. The observed seasonality indicates that depleted rains (δ18O=<-6 ‰) occur during the rainy season, associated to the great availability of humidity, transported mainly from Amazonia, associated with the South Atlantic Convergence Zone (ZCAS) and frontal systems, while enriched rains (δ18O=> -3 ‰) occur during the dry period, with the performance of the Cold Fronts (FF) and the formation of convective rains. The results presented and discussed in this paper contribute to the comprehension of seasonal variability in isotopic composition of precipitation, basic information for understanding about water movement, that include aquifer recharge, in state of São Paulo.
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spelling Variability of Isotopic Composition of Precipitation in the Central Region of the State of São PauloVariabilidade da Composição Isotópica da Precipitação na Região Central do Estado de São PauloPrecipitation and climate changeStable isotopesWater stable isotopes have been used as a tool in hydrometeorological studies, generating relevant information about the relationship between climate and groundwater recharge as well as determining surface water flows origin, contributing to the understanding of the consequences of climate change on the hydrological cycle. The present work presents the main climatic controls responsible for the variability in the precipitation monthly isotopic composition in the central region of São Paulo state, where areas of recharge of important aquifers of the Paraná Basin are located. Local meteoric water line (δ2H = 8.34 * δ18O + 15.71) indicates that the isotopic composition is influenced by a source of oceanic moisture and vapor recirculation processes along the displacement of air masses over the continent. The observed seasonality indicates that depleted rains (δ18O=<-6 ‰) occur during the rainy season, associated to the great availability of humidity, transported mainly from Amazonia, associated with the South Atlantic Convergence Zone (ZCAS) and frontal systems, while enriched rains (δ18O=> -3 ‰) occur during the dry period, with the performance of the Cold Fronts (FF) and the formation of convective rains. The results presented and discussed in this paper contribute to the comprehension of seasonal variability in isotopic composition of precipitation, basic information for understanding about water movement, that include aquifer recharge, in state of São Paulo.Universidade Estadual Paulista (UNESP) Centro de Estudos Ambientais, Campus Rio ClaroUniversidade de São Paulo (USP) Instituto de Astronomia Geofísica e Ciências Atmosféricas Departamento de Ciências Atmosféricas, SPUniversidade Estadual Paulista (UNESP) Centro de Estudos Ambientais, Campus Rio ClaroUniversidade Estadual Paulista (UNESP)Universidade de São Paulo (USP)Dos Santos, Vinícius [UNESP]Gastmans, Didier [UNESP]Santarosa, Lucas Vituri [UNESP]Batista, Ludmila Vianna [UNESP]Betancur, Sebastian Balbin [UNESP]De Oliverira, Marcelo Eduardo Dias [UNESP]Filho, Augusto José Pereira2025-04-29T19:14:10Z2019-04-02info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article171-181http://dx.doi.org/10.14295/ras.v33i2.29474Aguas Subterraneas, v. 33, n. 2, p. 171-181, 2019.2179-97840101-7004https://hdl.handle.net/11449/30229910.14295/ras.v33i2.294742-s2.0-85100077345Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporAguas Subterraneasinfo:eu-repo/semantics/openAccess2025-04-30T14:04:30Zoai:repositorio.unesp.br:11449/302299Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestrepositoriounesp@unesp.bropendoar:29462025-04-30T14:04:30Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
Variabilidade da Composição Isotópica da Precipitação na Região Central do Estado de São Paulo
title Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
spellingShingle Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
Dos Santos, Vinícius [UNESP]
Precipitation and climate change
Stable isotopes
title_short Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
title_full Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
title_fullStr Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
title_full_unstemmed Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
title_sort Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
author Dos Santos, Vinícius [UNESP]
author_facet Dos Santos, Vinícius [UNESP]
Gastmans, Didier [UNESP]
Santarosa, Lucas Vituri [UNESP]
Batista, Ludmila Vianna [UNESP]
Betancur, Sebastian Balbin [UNESP]
De Oliverira, Marcelo Eduardo Dias [UNESP]
Filho, Augusto José Pereira
author_role author
author2 Gastmans, Didier [UNESP]
Santarosa, Lucas Vituri [UNESP]
Batista, Ludmila Vianna [UNESP]
Betancur, Sebastian Balbin [UNESP]
De Oliverira, Marcelo Eduardo Dias [UNESP]
Filho, Augusto José Pereira
author2_role author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (UNESP)
Universidade de São Paulo (USP)
dc.contributor.author.fl_str_mv Dos Santos, Vinícius [UNESP]
Gastmans, Didier [UNESP]
Santarosa, Lucas Vituri [UNESP]
Batista, Ludmila Vianna [UNESP]
Betancur, Sebastian Balbin [UNESP]
De Oliverira, Marcelo Eduardo Dias [UNESP]
Filho, Augusto José Pereira
dc.subject.por.fl_str_mv Precipitation and climate change
Stable isotopes
topic Precipitation and climate change
Stable isotopes
description Water stable isotopes have been used as a tool in hydrometeorological studies, generating relevant information about the relationship between climate and groundwater recharge as well as determining surface water flows origin, contributing to the understanding of the consequences of climate change on the hydrological cycle. The present work presents the main climatic controls responsible for the variability in the precipitation monthly isotopic composition in the central region of São Paulo state, where areas of recharge of important aquifers of the Paraná Basin are located. Local meteoric water line (δ2H = 8.34 * δ18O + 15.71) indicates that the isotopic composition is influenced by a source of oceanic moisture and vapor recirculation processes along the displacement of air masses over the continent. The observed seasonality indicates that depleted rains (δ18O=<-6 ‰) occur during the rainy season, associated to the great availability of humidity, transported mainly from Amazonia, associated with the South Atlantic Convergence Zone (ZCAS) and frontal systems, while enriched rains (δ18O=> -3 ‰) occur during the dry period, with the performance of the Cold Fronts (FF) and the formation of convective rains. The results presented and discussed in this paper contribute to the comprehension of seasonal variability in isotopic composition of precipitation, basic information for understanding about water movement, that include aquifer recharge, in state of São Paulo.
publishDate 2019
dc.date.none.fl_str_mv 2019-04-02
2025-04-29T19:14:10Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.14295/ras.v33i2.29474
Aguas Subterraneas, v. 33, n. 2, p. 171-181, 2019.
2179-9784
0101-7004
https://hdl.handle.net/11449/302299
10.14295/ras.v33i2.29474
2-s2.0-85100077345
url http://dx.doi.org/10.14295/ras.v33i2.29474
https://hdl.handle.net/11449/302299
identifier_str_mv Aguas Subterraneas, v. 33, n. 2, p. 171-181, 2019.
2179-9784
0101-7004
10.14295/ras.v33i2.29474
2-s2.0-85100077345
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv Aguas Subterraneas
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 171-181
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv repositoriounesp@unesp.br
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