Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes

Detalhes bibliográficos
Autor(a) principal: Morán-Zuloaga, Daniel
Data de Publicação: 2018
Outros Autores: Ditas, Florian, Walter, David, Saturno, Jorge, Brito, Joel F., Carbone, Samara, Chi, Xuguang, Hrab? de Angelis, Isabella, Baars, Holger, H M Godoi, Ricardo, Heese, Birgit, A Holanda, Bruna, Lavric, J. V., Martin, Scot T., Ming, Jing, Pöhlker, Mira L., Ruckteschler, Nina, Su, Hang, Wang, Yaqiang, Wang, Qiaoqiao, Wang, Zhibin, Weber, Bettina, Wolff, Stefan, Artaxo, Paulo, Pöschl, Ulrich, Andreae, Meinrat O., Pöhlker, Christopher
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional do INPA
Texto Completo: https://repositorio.inpa.gov.br/handle/1/16231
Resumo: <p>In the Amazonian atmosphere, the aerosol coarse mode comprises a complex, diverse, and variable mixture of bioaerosols emitted from the rain forest ecosystem, long-range transported Saharan dust (we use Sahara as shorthand for the dust source regions in Africa north of the Equator), marine aerosols from the Atlantic Ocean, and coarse smoke particles from deforestation fires. For the rain forest, the coarse mode particles are of significance with respect to biogeochemical and hydrological cycling, as well as ecology and biogeography. However, knowledge on the physicochemical and biological properties as well as the ecological role of the Amazonian coarse mode is still sparse. This study presents results from multi-year coarse mode measurements at the remote Amazon Tall Tower Observatory (ATTO) site. It combines online aerosol observations, selected remote sensing and modeling results, as well as dedicated coarse mode sampling and analysis. The focal points of this study are a systematic characterization of aerosol coarse mode abundance and properties in the Amazonian atmosphere as well as a detailed analysis of the frequent, pulse-wise intrusion of African long-range transport (LRT) aerosols (comprising Saharan dust and African biomass burning smoke) into the Amazon Basin.</p><p>We find that, on a multi-year time scale, the Amazonian coarse mode maintains remarkably constant concentration levels (with 0.4 cmĝ'3 and 4.0 μg mĝ'3 in the wet vs. 1.2 cmĝ'3 and 6.5 μg mĝ'3 in the dry season) with rather weak seasonality (in terms of abundance and size spectrum), which is in stark contrast to the pronounced biomass burning-driven seasonality of the submicron aerosol population and related parameters. For most of the time, bioaerosol particles from the forest biome account for a major fraction of the coarse mode background population. However, from December to April there are episodic intrusions of African LRT aerosols, comprising Saharan dust, sea salt particles from the transatlantic passage, and African biomass burning smoke. Remarkably, during the core period of this LRT season (i.e., February-March), the presence of LRT influence, occurring as a sequence of pulse-like plumes, appears to be the norm rather than an exception. The LRT pulses increase the coarse mode concentrations drastically (up to 100 μg mĝ'3) and alter the coarse mode composition as well as its size spectrum. Efficient transport of the LRT plumes into the Amazon Basin takes place in response to specific mesoscale circulation patterns in combination with the episodic absence of rain-related aerosol scavenging en route. Based on a modeling study, we estimated a dust deposition flux of 5-10 kg haĝ'1 aĝ'1 in the region of the ATTO site. Furthermore, a chemical analysis quantified the substantial increase of crustal and sea salt elements under LRT conditions in comparison to the background coarse mode composition. With these results, we estimated the deposition fluxes of various elements that are considered as nutrients for the rain forest ecosystem. These estimates range from few g haĝ'1 aĝ'1 up to several hundreds of g haĝ'1 aĝ'1 in the ATTO region.</p><p>The long-term data presented here provide a statistically solid basis for future studies of the manifold aspects of the dynamic coarse mode aerosol cycling in the Amazon. Thus, it may help to understand its biogeochemical relevance in this ecosystem as well as to evaluate to what extent anthropogenic influences have altered the coarse mode cycling already.</p>. © 2018 Copernicus GmbH. All rights reserved.
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spelling Morán-Zuloaga, DanielDitas, FlorianWalter, DavidSaturno, JorgeBrito, Joel F.Carbone, SamaraChi, XuguangHrab? de Angelis, IsabellaBaars, HolgerH M Godoi, RicardoHeese, BirgitA Holanda, BrunaLavric, J. V.Martin, Scot T.Ming, JingPöhlker, Mira L.Ruckteschler, NinaSu, HangWang, YaqiangWang, QiaoqiaoWang, ZhibinWeber, BettinaWolff, StefanArtaxo, PauloPöschl, UlrichAndreae, Meinrat O.Pöhlker, Christopher2020-06-01T14:25:39Z2020-06-01T14:25:39Z2018https://repositorio.inpa.gov.br/handle/1/1623110.5194/acp-18-10055-2018<p>In the Amazonian atmosphere, the aerosol coarse mode comprises a complex, diverse, and variable mixture of bioaerosols emitted from the rain forest ecosystem, long-range transported Saharan dust (we use Sahara as shorthand for the dust source regions in Africa north of the Equator), marine aerosols from the Atlantic Ocean, and coarse smoke particles from deforestation fires. For the rain forest, the coarse mode particles are of significance with respect to biogeochemical and hydrological cycling, as well as ecology and biogeography. However, knowledge on the physicochemical and biological properties as well as the ecological role of the Amazonian coarse mode is still sparse. This study presents results from multi-year coarse mode measurements at the remote Amazon Tall Tower Observatory (ATTO) site. It combines online aerosol observations, selected remote sensing and modeling results, as well as dedicated coarse mode sampling and analysis. The focal points of this study are a systematic characterization of aerosol coarse mode abundance and properties in the Amazonian atmosphere as well as a detailed analysis of the frequent, pulse-wise intrusion of African long-range transport (LRT) aerosols (comprising Saharan dust and African biomass burning smoke) into the Amazon Basin.</p><p>We find that, on a multi-year time scale, the Amazonian coarse mode maintains remarkably constant concentration levels (with 0.4 cmĝ'3 and 4.0 μg mĝ'3 in the wet vs. 1.2 cmĝ'3 and 6.5 μg mĝ'3 in the dry season) with rather weak seasonality (in terms of abundance and size spectrum), which is in stark contrast to the pronounced biomass burning-driven seasonality of the submicron aerosol population and related parameters. For most of the time, bioaerosol particles from the forest biome account for a major fraction of the coarse mode background population. However, from December to April there are episodic intrusions of African LRT aerosols, comprising Saharan dust, sea salt particles from the transatlantic passage, and African biomass burning smoke. Remarkably, during the core period of this LRT season (i.e., February-March), the presence of LRT influence, occurring as a sequence of pulse-like plumes, appears to be the norm rather than an exception. The LRT pulses increase the coarse mode concentrations drastically (up to 100 μg mĝ'3) and alter the coarse mode composition as well as its size spectrum. Efficient transport of the LRT plumes into the Amazon Basin takes place in response to specific mesoscale circulation patterns in combination with the episodic absence of rain-related aerosol scavenging en route. Based on a modeling study, we estimated a dust deposition flux of 5-10 kg haĝ'1 aĝ'1 in the region of the ATTO site. Furthermore, a chemical analysis quantified the substantial increase of crustal and sea salt elements under LRT conditions in comparison to the background coarse mode composition. With these results, we estimated the deposition fluxes of various elements that are considered as nutrients for the rain forest ecosystem. These estimates range from few g haĝ'1 aĝ'1 up to several hundreds of g haĝ'1 aĝ'1 in the ATTO region.</p><p>The long-term data presented here provide a statistically solid basis for future studies of the manifold aspects of the dynamic coarse mode aerosol cycling in the Amazon. Thus, it may help to understand its biogeochemical relevance in this ecosystem as well as to evaluate to what extent anthropogenic influences have altered the coarse mode cycling already.</p>. © 2018 Copernicus GmbH. All rights reserved.Volume 18, Número 13, Pags. 10055-10088Attribution-NonCommercial-NoDerivs 3.0 Brazilhttp://creativecommons.org/licenses/by-nc-nd/3.0/br/info:eu-repo/semantics/openAccessAerosolAnthropogenic EffectAtmospheric PlumeBiogeochemistryBiomass-burningDustLong Range TransportRainforestAmazon BasinSaharaLong-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumesinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleAtmospheric Chemistry and Physicsengreponame:Repositório Institucional do INPAinstname:Instituto Nacional de Pesquisas da Amazônia (INPA)instacron:INPAORIGINALLong.pdfapplication/pdf17803196https://repositorio.inpa.gov.br/bitstream/1/16231/1/Long.pdfa099b2241a5dfc5a9f3185165cc1b295MD51CC-LICENSElicense_rdfapplication/octet-stream914https://repositorio.inpa.gov.br/bitstream/1/16231/2/license_rdf4d2950bda3d176f570a9f8b328dfbbefMD521/162312020-07-14 11:34:13.41oai:repositorio:1/16231Repositório de PublicaçõesPUBhttps://repositorio.inpa.gov.br/oai/requestopendoar:2020-07-14T15:34:13Repositório Institucional do INPA - Instituto Nacional de Pesquisas da Amazônia (INPA)false
dc.title.en.fl_str_mv Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
title Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
spellingShingle Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
Morán-Zuloaga, Daniel
Aerosol
Anthropogenic Effect
Atmospheric Plume
Biogeochemistry
Biomass-burning
Dust
Long Range Transport
Rainforest
Amazon Basin
Sahara
title_short Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
title_full Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
title_fullStr Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
title_full_unstemmed Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
title_sort Long-term study on coarse mode aerosols in the Amazon rain forest with the frequent intrusion of Saharan dust plumes
author Morán-Zuloaga, Daniel
author_facet Morán-Zuloaga, Daniel
Ditas, Florian
Walter, David
Saturno, Jorge
Brito, Joel F.
Carbone, Samara
Chi, Xuguang
Hrab? de Angelis, Isabella
Baars, Holger
H M Godoi, Ricardo
Heese, Birgit
A Holanda, Bruna
Lavric, J. V.
Martin, Scot T.
Ming, Jing
Pöhlker, Mira L.
Ruckteschler, Nina
Su, Hang
Wang, Yaqiang
Wang, Qiaoqiao
Wang, Zhibin
Weber, Bettina
Wolff, Stefan
Artaxo, Paulo
Pöschl, Ulrich
Andreae, Meinrat O.
Pöhlker, Christopher
author_role author
author2 Ditas, Florian
Walter, David
Saturno, Jorge
Brito, Joel F.
Carbone, Samara
Chi, Xuguang
Hrab? de Angelis, Isabella
Baars, Holger
H M Godoi, Ricardo
Heese, Birgit
A Holanda, Bruna
Lavric, J. V.
Martin, Scot T.
Ming, Jing
Pöhlker, Mira L.
Ruckteschler, Nina
Su, Hang
Wang, Yaqiang
Wang, Qiaoqiao
Wang, Zhibin
Weber, Bettina
Wolff, Stefan
Artaxo, Paulo
Pöschl, Ulrich
Andreae, Meinrat O.
Pöhlker, Christopher
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Morán-Zuloaga, Daniel
Ditas, Florian
Walter, David
Saturno, Jorge
Brito, Joel F.
Carbone, Samara
Chi, Xuguang
Hrab? de Angelis, Isabella
Baars, Holger
H M Godoi, Ricardo
Heese, Birgit
A Holanda, Bruna
Lavric, J. V.
Martin, Scot T.
Ming, Jing
Pöhlker, Mira L.
Ruckteschler, Nina
Su, Hang
Wang, Yaqiang
Wang, Qiaoqiao
Wang, Zhibin
Weber, Bettina
Wolff, Stefan
Artaxo, Paulo
Pöschl, Ulrich
Andreae, Meinrat O.
Pöhlker, Christopher
dc.subject.eng.fl_str_mv Aerosol
Anthropogenic Effect
Atmospheric Plume
Biogeochemistry
Biomass-burning
Dust
Long Range Transport
Rainforest
Amazon Basin
Sahara
topic Aerosol
Anthropogenic Effect
Atmospheric Plume
Biogeochemistry
Biomass-burning
Dust
Long Range Transport
Rainforest
Amazon Basin
Sahara
description <p>In the Amazonian atmosphere, the aerosol coarse mode comprises a complex, diverse, and variable mixture of bioaerosols emitted from the rain forest ecosystem, long-range transported Saharan dust (we use Sahara as shorthand for the dust source regions in Africa north of the Equator), marine aerosols from the Atlantic Ocean, and coarse smoke particles from deforestation fires. For the rain forest, the coarse mode particles are of significance with respect to biogeochemical and hydrological cycling, as well as ecology and biogeography. However, knowledge on the physicochemical and biological properties as well as the ecological role of the Amazonian coarse mode is still sparse. This study presents results from multi-year coarse mode measurements at the remote Amazon Tall Tower Observatory (ATTO) site. It combines online aerosol observations, selected remote sensing and modeling results, as well as dedicated coarse mode sampling and analysis. The focal points of this study are a systematic characterization of aerosol coarse mode abundance and properties in the Amazonian atmosphere as well as a detailed analysis of the frequent, pulse-wise intrusion of African long-range transport (LRT) aerosols (comprising Saharan dust and African biomass burning smoke) into the Amazon Basin.</p><p>We find that, on a multi-year time scale, the Amazonian coarse mode maintains remarkably constant concentration levels (with 0.4 cmĝ'3 and 4.0 μg mĝ'3 in the wet vs. 1.2 cmĝ'3 and 6.5 μg mĝ'3 in the dry season) with rather weak seasonality (in terms of abundance and size spectrum), which is in stark contrast to the pronounced biomass burning-driven seasonality of the submicron aerosol population and related parameters. For most of the time, bioaerosol particles from the forest biome account for a major fraction of the coarse mode background population. However, from December to April there are episodic intrusions of African LRT aerosols, comprising Saharan dust, sea salt particles from the transatlantic passage, and African biomass burning smoke. Remarkably, during the core period of this LRT season (i.e., February-March), the presence of LRT influence, occurring as a sequence of pulse-like plumes, appears to be the norm rather than an exception. The LRT pulses increase the coarse mode concentrations drastically (up to 100 μg mĝ'3) and alter the coarse mode composition as well as its size spectrum. Efficient transport of the LRT plumes into the Amazon Basin takes place in response to specific mesoscale circulation patterns in combination with the episodic absence of rain-related aerosol scavenging en route. Based on a modeling study, we estimated a dust deposition flux of 5-10 kg haĝ'1 aĝ'1 in the region of the ATTO site. Furthermore, a chemical analysis quantified the substantial increase of crustal and sea salt elements under LRT conditions in comparison to the background coarse mode composition. With these results, we estimated the deposition fluxes of various elements that are considered as nutrients for the rain forest ecosystem. These estimates range from few g haĝ'1 aĝ'1 up to several hundreds of g haĝ'1 aĝ'1 in the ATTO region.</p><p>The long-term data presented here provide a statistically solid basis for future studies of the manifold aspects of the dynamic coarse mode aerosol cycling in the Amazon. Thus, it may help to understand its biogeochemical relevance in this ecosystem as well as to evaluate to what extent anthropogenic influences have altered the coarse mode cycling already.</p>. © 2018 Copernicus GmbH. All rights reserved.
publishDate 2018
dc.date.issued.fl_str_mv 2018
dc.date.accessioned.fl_str_mv 2020-06-01T14:25:39Z
dc.date.available.fl_str_mv 2020-06-01T14:25:39Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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status_str publishedVersion
dc.identifier.uri.fl_str_mv https://repositorio.inpa.gov.br/handle/1/16231
dc.identifier.doi.none.fl_str_mv 10.5194/acp-18-10055-2018
url https://repositorio.inpa.gov.br/handle/1/16231
identifier_str_mv 10.5194/acp-18-10055-2018
dc.language.iso.fl_str_mv eng
language eng
dc.relation.ispartof.pt_BR.fl_str_mv Volume 18, Número 13, Pags. 10055-10088
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http://creativecommons.org/licenses/by-nc-nd/3.0/br/
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rights_invalid_str_mv Attribution-NonCommercial-NoDerivs 3.0 Brazil
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eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Atmospheric Chemistry and Physics
publisher.none.fl_str_mv Atmospheric Chemistry and Physics
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