Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions

Autores
Tidiga, Mariam; Berthet, Gwenaël; Jegou, Fabrice; Bossolasco, Adriana Gabriela; Kloss, Corinna; Bègue, Nelson; Renard, Jean-Baptiste; Vernier, Jean-Paul; Clarisse, Lieven; Taha, Ghassan; Portafaix, Thierry; Metzger, Jean-Marc; Payen, Guillaume
Año de publicación
2021
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The cumulative impacts of frequent moderate-magnitude eruptions on stratospheric aerosolswere identified among the factors in recent decadal climate trends. Moderate volcanic eruptionsare a recurrent source of sulfur dioxide (SO2) in the Upper Troposphere and Lower Stratosphere(UTLS) region and the resulting formation of sulfuric acid aerosol particles from the SO2 emittedprovides sites for chemical reactions leading to enhancement of stratospheric optical depth(SAOD) and ozone depletion. Modelling properly the volcanic aerosol content and its evolution inthis region is important for radiative impact issues. In this work, we explore the variability of thetropical UTLS aerosol content between 2013 and 2019, a period which was particularly impactedby moderate tropical and mid-latitude volcanic eruptions. For that purpose, space-borneobservations from OMPS (version 2, datasets from GES DISC), and IASI, together with simulationsby the Whole Atmosphere Community Climate Model (WACCM) coupled with the CommunityAerosol and Radiation Model for Atmospheres (CARMA), are used. Different model sensitiveexperiments, particularly for the injection altitude and timing, have been conducted to evaluatehow the model captures the aerosol plume in terms of content, optical and microphysicalproperties, transport and residence time. We find that the decay of the Calbuco and Kelud plumesobserved by OMPS version 2 is well reproduced by the model. Comparisons with unique datasetsin the tropical southern hemisphere from the NDACC Maïdo observatory (Reunion Island, France,20.5°S, 55.5°E) show good agreement between the lidar SAOD observations and WACCM-CARMASAOD simulations although we observe a difference in the altitude of the maximum aerosolconcentration between the model and the in situ profile after Calbuco eruption in April 2015. Aparticular focus is also made on recent eruptions like Raikoke, Ambae and Ulawun. The plume ofthe Ambae volcano (15°S, 167°E) which erupted in July 2018 is shown to propagate to the northernhemisphere with some influence until summer 2019 in the Asian monsoon region. For the year2019, we investigate how the Ulawun (5°S, 151°E; ~0.14 Tg of SO2) tropical eruption and theRaikoke mid-latitude eruption (48°N, 153°E; ~1.5Tg of SO2), have influenced the aerosol burden in the tropics.
Fil: Tidiga, Mariam. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Berthet, Gwenaël. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Jegou, Fabrice. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Bossolasco, Adriana Gabriela. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; Argentina. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Kloss, Corinna. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Bègue, Nelson. Laboratoire de L'atmosphère Et Des Cyclones; Francia
Fil: Renard, Jean-Baptiste. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Vernier, Jean-Paul. National Institute Of Aerospace.; Estados Unidos
Fil: Clarisse, Lieven. Université Libre de Bruxelles; Bélgica
Fil: Taha, Ghassan. Universities Space Research Association; Estados Unidos
Fil: Portafaix, Thierry. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
Fil: Metzger, Jean-Marc. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
Fil: Payen, Guillaume. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
General Assembly 2021 of the European Geosciences Union
Viena
Austria
Copernicus Meetings
Materia
Volcanic Eruptions
WACCAM simulations
Stratospheric Aerosols
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/243586

id CONICETDig_08e035b37b22b5f080a370a01f507b29
oai_identifier_str oai:ri.conicet.gov.ar:11336/243586
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptionsTidiga, MariamBerthet, GwenaëlJegou, FabriceBossolasco, Adriana GabrielaKloss, CorinnaBègue, NelsonRenard, Jean-BaptisteVernier, Jean-PaulClarisse, LievenTaha, GhassanPortafaix, ThierryMetzger, Jean-MarcPayen, GuillaumeVolcanic EruptionsWACCAM simulationsStratospheric Aerosolshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The cumulative impacts of frequent moderate-magnitude eruptions on stratospheric aerosolswere identified among the factors in recent decadal climate trends. Moderate volcanic eruptionsare a recurrent source of sulfur dioxide (SO2) in the Upper Troposphere and Lower Stratosphere(UTLS) region and the resulting formation of sulfuric acid aerosol particles from the SO2 emittedprovides sites for chemical reactions leading to enhancement of stratospheric optical depth(SAOD) and ozone depletion. Modelling properly the volcanic aerosol content and its evolution inthis region is important for radiative impact issues. In this work, we explore the variability of thetropical UTLS aerosol content between 2013 and 2019, a period which was particularly impactedby moderate tropical and mid-latitude volcanic eruptions. For that purpose, space-borneobservations from OMPS (version 2, datasets from GES DISC), and IASI, together with simulationsby the Whole Atmosphere Community Climate Model (WACCM) coupled with the CommunityAerosol and Radiation Model for Atmospheres (CARMA), are used. Different model sensitiveexperiments, particularly for the injection altitude and timing, have been conducted to evaluatehow the model captures the aerosol plume in terms of content, optical and microphysicalproperties, transport and residence time. We find that the decay of the Calbuco and Kelud plumesobserved by OMPS version 2 is well reproduced by the model. Comparisons with unique datasetsin the tropical southern hemisphere from the NDACC Maïdo observatory (Reunion Island, France,20.5°S, 55.5°E) show good agreement between the lidar SAOD observations and WACCM-CARMASAOD simulations although we observe a difference in the altitude of the maximum aerosolconcentration between the model and the in situ profile after Calbuco eruption in April 2015. Aparticular focus is also made on recent eruptions like Raikoke, Ambae and Ulawun. The plume ofthe Ambae volcano (15°S, 167°E) which erupted in July 2018 is shown to propagate to the northernhemisphere with some influence until summer 2019 in the Asian monsoon region. For the year2019, we investigate how the Ulawun (5°S, 151°E; ~0.14 Tg of SO2) tropical eruption and theRaikoke mid-latitude eruption (48°N, 153°E; ~1.5Tg of SO2), have influenced the aerosol burden in the tropics.Fil: Tidiga, Mariam. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Berthet, Gwenaël. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Jegou, Fabrice. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Bossolasco, Adriana Gabriela. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; Argentina. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Kloss, Corinna. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Bègue, Nelson. Laboratoire de L'atmosphère Et Des Cyclones; FranciaFil: Renard, Jean-Baptiste. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; FranciaFil: Vernier, Jean-Paul. National Institute Of Aerospace.; Estados UnidosFil: Clarisse, Lieven. Université Libre de Bruxelles; BélgicaFil: Taha, Ghassan. Universities Space Research Association; Estados UnidosFil: Portafaix, Thierry. Laboratoire de L'atmosphère Et Des Cyclones; ReuniónFil: Metzger, Jean-Marc. Laboratoire de L'atmosphère Et Des Cyclones; ReuniónFil: Payen, Guillaume. Laboratoire de L'atmosphère Et Des Cyclones; ReuniónGeneral Assembly 2021 of the European Geosciences UnionVienaAustriaCopernicus MeetingsCopernicus Publications2021info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectOtroBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/243586Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions; General Assembly 2021 of the European Geosciences Union; Viena; Austria; 2021; 1-2CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://meetingorganizer.copernicus.org/EGU21/EGU21-2690.htmlinfo:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu21-2690Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:57:37Zoai:ri.conicet.gov.ar:11336/243586instacron: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 09:57:37.813CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
title Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
spellingShingle Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
Tidiga, Mariam
Volcanic Eruptions
WACCAM simulations
Stratospheric Aerosols
title_short Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
title_full Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
title_fullStr Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
title_full_unstemmed Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
title_sort Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions
dc.creator.none.fl_str_mv Tidiga, Mariam
Berthet, Gwenaël
Jegou, Fabrice
Bossolasco, Adriana Gabriela
Kloss, Corinna
Bègue, Nelson
Renard, Jean-Baptiste
Vernier, Jean-Paul
Clarisse, Lieven
Taha, Ghassan
Portafaix, Thierry
Metzger, Jean-Marc
Payen, Guillaume
author Tidiga, Mariam
author_facet Tidiga, Mariam
Berthet, Gwenaël
Jegou, Fabrice
Bossolasco, Adriana Gabriela
Kloss, Corinna
Bègue, Nelson
Renard, Jean-Baptiste
Vernier, Jean-Paul
Clarisse, Lieven
Taha, Ghassan
Portafaix, Thierry
Metzger, Jean-Marc
Payen, Guillaume
author_role author
author2 Berthet, Gwenaël
Jegou, Fabrice
Bossolasco, Adriana Gabriela
Kloss, Corinna
Bègue, Nelson
Renard, Jean-Baptiste
Vernier, Jean-Paul
Clarisse, Lieven
Taha, Ghassan
Portafaix, Thierry
Metzger, Jean-Marc
Payen, Guillaume
author2_role author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Volcanic Eruptions
WACCAM simulations
Stratospheric Aerosols
topic Volcanic Eruptions
WACCAM simulations
Stratospheric Aerosols
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The cumulative impacts of frequent moderate-magnitude eruptions on stratospheric aerosolswere identified among the factors in recent decadal climate trends. Moderate volcanic eruptionsare a recurrent source of sulfur dioxide (SO2) in the Upper Troposphere and Lower Stratosphere(UTLS) region and the resulting formation of sulfuric acid aerosol particles from the SO2 emittedprovides sites for chemical reactions leading to enhancement of stratospheric optical depth(SAOD) and ozone depletion. Modelling properly the volcanic aerosol content and its evolution inthis region is important for radiative impact issues. In this work, we explore the variability of thetropical UTLS aerosol content between 2013 and 2019, a period which was particularly impactedby moderate tropical and mid-latitude volcanic eruptions. For that purpose, space-borneobservations from OMPS (version 2, datasets from GES DISC), and IASI, together with simulationsby the Whole Atmosphere Community Climate Model (WACCM) coupled with the CommunityAerosol and Radiation Model for Atmospheres (CARMA), are used. Different model sensitiveexperiments, particularly for the injection altitude and timing, have been conducted to evaluatehow the model captures the aerosol plume in terms of content, optical and microphysicalproperties, transport and residence time. We find that the decay of the Calbuco and Kelud plumesobserved by OMPS version 2 is well reproduced by the model. Comparisons with unique datasetsin the tropical southern hemisphere from the NDACC Maïdo observatory (Reunion Island, France,20.5°S, 55.5°E) show good agreement between the lidar SAOD observations and WACCM-CARMASAOD simulations although we observe a difference in the altitude of the maximum aerosolconcentration between the model and the in situ profile after Calbuco eruption in April 2015. Aparticular focus is also made on recent eruptions like Raikoke, Ambae and Ulawun. The plume ofthe Ambae volcano (15°S, 167°E) which erupted in July 2018 is shown to propagate to the northernhemisphere with some influence until summer 2019 in the Asian monsoon region. For the year2019, we investigate how the Ulawun (5°S, 151°E; ~0.14 Tg of SO2) tropical eruption and theRaikoke mid-latitude eruption (48°N, 153°E; ~1.5Tg of SO2), have influenced the aerosol burden in the tropics.
Fil: Tidiga, Mariam. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Berthet, Gwenaël. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Jegou, Fabrice. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Bossolasco, Adriana Gabriela. Universidad Nacional de Tucumán. Instituto de Física del Noroeste Argentino. - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet Noa Sur. Instituto de Física del Noroeste Argentino; Argentina. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Kloss, Corinna. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Bègue, Nelson. Laboratoire de L'atmosphère Et Des Cyclones; Francia
Fil: Renard, Jean-Baptiste. Laboratoire de Physique de Chimie de l’Environnement et de l’Espace; Francia
Fil: Vernier, Jean-Paul. National Institute Of Aerospace.; Estados Unidos
Fil: Clarisse, Lieven. Université Libre de Bruxelles; Bélgica
Fil: Taha, Ghassan. Universities Space Research Association; Estados Unidos
Fil: Portafaix, Thierry. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
Fil: Metzger, Jean-Marc. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
Fil: Payen, Guillaume. Laboratoire de L'atmosphère Et Des Cyclones; Reunión
General Assembly 2021 of the European Geosciences Union
Viena
Austria
Copernicus Meetings
description The cumulative impacts of frequent moderate-magnitude eruptions on stratospheric aerosolswere identified among the factors in recent decadal climate trends. Moderate volcanic eruptionsare a recurrent source of sulfur dioxide (SO2) in the Upper Troposphere and Lower Stratosphere(UTLS) region and the resulting formation of sulfuric acid aerosol particles from the SO2 emittedprovides sites for chemical reactions leading to enhancement of stratospheric optical depth(SAOD) and ozone depletion. Modelling properly the volcanic aerosol content and its evolution inthis region is important for radiative impact issues. In this work, we explore the variability of thetropical UTLS aerosol content between 2013 and 2019, a period which was particularly impactedby moderate tropical and mid-latitude volcanic eruptions. For that purpose, space-borneobservations from OMPS (version 2, datasets from GES DISC), and IASI, together with simulationsby the Whole Atmosphere Community Climate Model (WACCM) coupled with the CommunityAerosol and Radiation Model for Atmospheres (CARMA), are used. Different model sensitiveexperiments, particularly for the injection altitude and timing, have been conducted to evaluatehow the model captures the aerosol plume in terms of content, optical and microphysicalproperties, transport and residence time. We find that the decay of the Calbuco and Kelud plumesobserved by OMPS version 2 is well reproduced by the model. Comparisons with unique datasetsin the tropical southern hemisphere from the NDACC Maïdo observatory (Reunion Island, France,20.5°S, 55.5°E) show good agreement between the lidar SAOD observations and WACCM-CARMASAOD simulations although we observe a difference in the altitude of the maximum aerosolconcentration between the model and the in situ profile after Calbuco eruption in April 2015. Aparticular focus is also made on recent eruptions like Raikoke, Ambae and Ulawun. The plume ofthe Ambae volcano (15°S, 167°E) which erupted in July 2018 is shown to propagate to the northernhemisphere with some influence until summer 2019 in the Asian monsoon region. For the year2019, we investigate how the Ulawun (5°S, 151°E; ~0.14 Tg of SO2) tropical eruption and theRaikoke mid-latitude eruption (48°N, 153°E; ~1.5Tg of SO2), have influenced the aerosol burden in the tropics.
publishDate 2021
dc.date.none.fl_str_mv 2021
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Otro
Book
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/243586
Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions; General Assembly 2021 of the European Geosciences Union; Viena; Austria; 2021; 1-2
CONICET Digital
CONICET
url http://hdl.handle.net/11336/243586
identifier_str_mv Variability of the aerosol content in the tropical lower stratosphere from 2013 to 2019 as influenced by moderate volcanic eruptions; General Assembly 2021 of the European Geosciences Union; Viena; Austria; 2021; 1-2
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://meetingorganizer.copernicus.org/EGU21/EGU21-2690.html
info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu21-2690
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.coverage.none.fl_str_mv Internacional
dc.publisher.none.fl_str_mv Copernicus Publications
publisher.none.fl_str_mv Copernicus Publications
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1842269473257553920
score 13.13397