Spatial and Temporal Variability of Iodine in Aerosol
- Autores
- Gómez Martín, Juan Carlos; Saiz López, Alfonso; Cuevas, Carlos Alberto; Fernandez, Rafael Pedro; Gilfedder, Benjamin; Weller, Rolf; Baker, Alex R.; Droste, Elise; Lai, Senchao
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- In this work, we describe the compilation and homogenization of an extensive data set of aerosol iodine field observations in the period between 1963 and 2018 and we discuss its spatial and temporal dependences by comparison with CAM-Chem model simulations. A close to linear relationship between soluble and total iodine in aerosol is found (∼80% aerosol iodine is soluble), which enables converting a large subset of measurements of soluble iodine into total iodine. The resulting data set shows a distinct latitudinal dependence, with an enhancement toward the Northern Hemisphere (NH) tropics and lower values toward the poles. This behavior, which has been predicted by atmospheric models to depend on the global distribution of the main oceanic iodine source (which in turn depends on the reaction of ozone with aqueous iodide on the sea water-air interface, generating gas-phase I2 and HOI), is confirmed here by field observations for the first time. Longitudinally, there is some indication of a wave-one profile in the tropics, which peaks in the Atlantic and shows a minimum in the Pacific. New data from Antarctica show that the south polar seasonal variation of iodine in aerosol mirrors that observed previously in the Arctic, with two equinoctial maxima and the dominant maximum occurring in spring. While no clear seasonal variability is observed in NH middle latitudes, there is an indication of different seasonal cycles in the NH tropical Atlantic and Pacific. Long-term trends cannot be unambiguously established as a result of inhomogeneous time and spatial coverage and analytical methods.
Fil: Gómez Martín, Juan Carlos. Consejo Superior de Investigaciones Científicas; España. Instituto de Astrofísica de Andalucía ; España
Fil: Saiz López, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; España
Fil: Cuevas, Carlos Alberto. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; España
Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina
Fil: Gilfedder, Benjamin. University of Bayreuth; Alemania
Fil: Weller, Rolf. Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung; Alemania
Fil: Baker, Alex R.. University of East Anglia; Reino Unido
Fil: Droste, Elise. University of East Anglia; Reino Unido. Wageningen University; Países Bajos
Fil: Lai, Senchao. South China University of Technology; China - Materia
-
AEROSOL COMPOSITION
ATMOSPHERIC IODINE
IODINE SOURCES - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/211421
Ver los metadatos del registro completo
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Spatial and Temporal Variability of Iodine in AerosolGómez Martín, Juan CarlosSaiz López, AlfonsoCuevas, Carlos AlbertoFernandez, Rafael PedroGilfedder, BenjaminWeller, RolfBaker, Alex R.Droste, EliseLai, SenchaoAEROSOL COMPOSITIONATMOSPHERIC IODINEIODINE SOURCEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1In this work, we describe the compilation and homogenization of an extensive data set of aerosol iodine field observations in the period between 1963 and 2018 and we discuss its spatial and temporal dependences by comparison with CAM-Chem model simulations. A close to linear relationship between soluble and total iodine in aerosol is found (∼80% aerosol iodine is soluble), which enables converting a large subset of measurements of soluble iodine into total iodine. The resulting data set shows a distinct latitudinal dependence, with an enhancement toward the Northern Hemisphere (NH) tropics and lower values toward the poles. This behavior, which has been predicted by atmospheric models to depend on the global distribution of the main oceanic iodine source (which in turn depends on the reaction of ozone with aqueous iodide on the sea water-air interface, generating gas-phase I2 and HOI), is confirmed here by field observations for the first time. Longitudinally, there is some indication of a wave-one profile in the tropics, which peaks in the Atlantic and shows a minimum in the Pacific. New data from Antarctica show that the south polar seasonal variation of iodine in aerosol mirrors that observed previously in the Arctic, with two equinoctial maxima and the dominant maximum occurring in spring. While no clear seasonal variability is observed in NH middle latitudes, there is an indication of different seasonal cycles in the NH tropical Atlantic and Pacific. Long-term trends cannot be unambiguously established as a result of inhomogeneous time and spatial coverage and analytical methods.Fil: Gómez Martín, Juan Carlos. Consejo Superior de Investigaciones Científicas; España. Instituto de Astrofísica de Andalucía ; EspañaFil: Saiz López, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; EspañaFil: Cuevas, Carlos Alberto. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; EspañaFil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; ArgentinaFil: Gilfedder, Benjamin. University of Bayreuth; AlemaniaFil: Weller, Rolf. Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung; AlemaniaFil: Baker, Alex R.. University of East Anglia; Reino UnidoFil: Droste, Elise. University of East Anglia; Reino Unido. Wageningen University; Países BajosFil: Lai, Senchao. South China University of Technology; ChinaBlackwell Publishing2021-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/211421Gómez Martín, Juan Carlos; Saiz López, Alfonso; Cuevas, Carlos Alberto; Fernandez, Rafael Pedro; Gilfedder, Benjamin; et al.; Spatial and Temporal Variability of Iodine in Aerosol; Blackwell Publishing; Journal of Geophysical Research: Atmospheres; 126; 9; 5-2021; 1-232169-8996CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020JD034410info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JD034410info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:07:00Zoai:ri.conicet.gov.ar:11336/211421instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:07:01.21CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Spatial and Temporal Variability of Iodine in Aerosol |
title |
Spatial and Temporal Variability of Iodine in Aerosol |
spellingShingle |
Spatial and Temporal Variability of Iodine in Aerosol Gómez Martín, Juan Carlos AEROSOL COMPOSITION ATMOSPHERIC IODINE IODINE SOURCES |
title_short |
Spatial and Temporal Variability of Iodine in Aerosol |
title_full |
Spatial and Temporal Variability of Iodine in Aerosol |
title_fullStr |
Spatial and Temporal Variability of Iodine in Aerosol |
title_full_unstemmed |
Spatial and Temporal Variability of Iodine in Aerosol |
title_sort |
Spatial and Temporal Variability of Iodine in Aerosol |
dc.creator.none.fl_str_mv |
Gómez Martín, Juan Carlos Saiz López, Alfonso Cuevas, Carlos Alberto Fernandez, Rafael Pedro Gilfedder, Benjamin Weller, Rolf Baker, Alex R. Droste, Elise Lai, Senchao |
author |
Gómez Martín, Juan Carlos |
author_facet |
Gómez Martín, Juan Carlos Saiz López, Alfonso Cuevas, Carlos Alberto Fernandez, Rafael Pedro Gilfedder, Benjamin Weller, Rolf Baker, Alex R. Droste, Elise Lai, Senchao |
author_role |
author |
author2 |
Saiz López, Alfonso Cuevas, Carlos Alberto Fernandez, Rafael Pedro Gilfedder, Benjamin Weller, Rolf Baker, Alex R. Droste, Elise Lai, Senchao |
author2_role |
author author author author author author author author |
dc.subject.none.fl_str_mv |
AEROSOL COMPOSITION ATMOSPHERIC IODINE IODINE SOURCES |
topic |
AEROSOL COMPOSITION ATMOSPHERIC IODINE IODINE SOURCES |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
In this work, we describe the compilation and homogenization of an extensive data set of aerosol iodine field observations in the period between 1963 and 2018 and we discuss its spatial and temporal dependences by comparison with CAM-Chem model simulations. A close to linear relationship between soluble and total iodine in aerosol is found (∼80% aerosol iodine is soluble), which enables converting a large subset of measurements of soluble iodine into total iodine. The resulting data set shows a distinct latitudinal dependence, with an enhancement toward the Northern Hemisphere (NH) tropics and lower values toward the poles. This behavior, which has been predicted by atmospheric models to depend on the global distribution of the main oceanic iodine source (which in turn depends on the reaction of ozone with aqueous iodide on the sea water-air interface, generating gas-phase I2 and HOI), is confirmed here by field observations for the first time. Longitudinally, there is some indication of a wave-one profile in the tropics, which peaks in the Atlantic and shows a minimum in the Pacific. New data from Antarctica show that the south polar seasonal variation of iodine in aerosol mirrors that observed previously in the Arctic, with two equinoctial maxima and the dominant maximum occurring in spring. While no clear seasonal variability is observed in NH middle latitudes, there is an indication of different seasonal cycles in the NH tropical Atlantic and Pacific. Long-term trends cannot be unambiguously established as a result of inhomogeneous time and spatial coverage and analytical methods. Fil: Gómez Martín, Juan Carlos. Consejo Superior de Investigaciones Científicas; España. Instituto de Astrofísica de Andalucía ; España Fil: Saiz López, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; España Fil: Cuevas, Carlos Alberto. Consejo Superior de Investigaciones Científicas. Instituto de Química Física "Rocasolano"; España Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina Fil: Gilfedder, Benjamin. University of Bayreuth; Alemania Fil: Weller, Rolf. Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung; Alemania Fil: Baker, Alex R.. University of East Anglia; Reino Unido Fil: Droste, Elise. University of East Anglia; Reino Unido. Wageningen University; Países Bajos Fil: Lai, Senchao. South China University of Technology; China |
description |
In this work, we describe the compilation and homogenization of an extensive data set of aerosol iodine field observations in the period between 1963 and 2018 and we discuss its spatial and temporal dependences by comparison with CAM-Chem model simulations. A close to linear relationship between soluble and total iodine in aerosol is found (∼80% aerosol iodine is soluble), which enables converting a large subset of measurements of soluble iodine into total iodine. The resulting data set shows a distinct latitudinal dependence, with an enhancement toward the Northern Hemisphere (NH) tropics and lower values toward the poles. This behavior, which has been predicted by atmospheric models to depend on the global distribution of the main oceanic iodine source (which in turn depends on the reaction of ozone with aqueous iodide on the sea water-air interface, generating gas-phase I2 and HOI), is confirmed here by field observations for the first time. Longitudinally, there is some indication of a wave-one profile in the tropics, which peaks in the Atlantic and shows a minimum in the Pacific. New data from Antarctica show that the south polar seasonal variation of iodine in aerosol mirrors that observed previously in the Arctic, with two equinoctial maxima and the dominant maximum occurring in spring. While no clear seasonal variability is observed in NH middle latitudes, there is an indication of different seasonal cycles in the NH tropical Atlantic and Pacific. Long-term trends cannot be unambiguously established as a result of inhomogeneous time and spatial coverage and analytical methods. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-05 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/211421 Gómez Martín, Juan Carlos; Saiz López, Alfonso; Cuevas, Carlos Alberto; Fernandez, Rafael Pedro; Gilfedder, Benjamin; et al.; Spatial and Temporal Variability of Iodine in Aerosol; Blackwell Publishing; Journal of Geophysical Research: Atmospheres; 126; 9; 5-2021; 1-23 2169-8996 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/211421 |
identifier_str_mv |
Gómez Martín, Juan Carlos; Saiz López, Alfonso; Cuevas, Carlos Alberto; Fernandez, Rafael Pedro; Gilfedder, Benjamin; et al.; Spatial and Temporal Variability of Iodine in Aerosol; Blackwell Publishing; Journal of Geophysical Research: Atmospheres; 126; 9; 5-2021; 1-23 2169-8996 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020JD034410 info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JD034410 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Blackwell Publishing |
publisher.none.fl_str_mv |
Blackwell Publishing |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.13397 |