Variability of Isotopic Composition of Precipitation in the Central Region of the State of São Paulo
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Publication Date: | 2019 |
Other Authors: | , , , , , |
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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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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1834482919482064896 |