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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/243586
Ver los metadatos del registro completo
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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 |
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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 |
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publishedVersion |
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conferenceObject |
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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 |
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eng |
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eng |
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