The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives

Abstract Among the regions of the Southern Ocean, the northern Antarctic Peninsula (NAP) has emerged as a hotspot of climate change investigation. Nonetheless, studies have indicated issues and knowledge gaps that must be addressed to expand the understanding of the carbonate system in the region. T...

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Main Authors: IOLE B.M. ORSELLI, ANDRÉA C.O. CARVALHO, THIAGO MONTEIRO, BRENDON Y. DAMINI, MARIAH DE CARVALHO-BORGES, CÍNTIA ALBUQUERQUE, RODRIGO KERR
Format: Article
Language:English
Published: Academia Brasileira de Ciências 2022-05-01
Series:Anais da Academia Brasileira de Ciências
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652022000201119&lng=en&tlng=en
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author IOLE B.M. ORSELLI
ANDRÉA C.O. CARVALHO
THIAGO MONTEIRO
BRENDON Y. DAMINI
MARIAH DE CARVALHO-BORGES
CÍNTIA ALBUQUERQUE
RODRIGO KERR
author_facet IOLE B.M. ORSELLI
ANDRÉA C.O. CARVALHO
THIAGO MONTEIRO
BRENDON Y. DAMINI
MARIAH DE CARVALHO-BORGES
CÍNTIA ALBUQUERQUE
RODRIGO KERR
author_sort IOLE B.M. ORSELLI
collection DOAJ
description Abstract Among the regions of the Southern Ocean, the northern Antarctic Peninsula (NAP) has emerged as a hotspot of climate change investigation. Nonetheless, studies have indicated issues and knowledge gaps that must be addressed to expand the understanding of the carbonate system in the region. Therefore, we focused on identifying current knowledge about sea-air CO2 fluxes (FCO2), anthropogenic carbon (Cant) and ocean acidification along NAP and provide a better comprehension of the key physical processes controlling the carbonate system. Regarding physical dynamics, we discuss the role of water masses formation, climate modes, upwelling and intrusions of Circumpolar Deep Water, and mesoscale processes. For FCO2, we show that the summer season corresponds to a strong sink in coastal areas, leading to CO2 uptake that is greater than or equal to that of the open ocean. We highlight that the prevalence of summer studies prevents comprehending processes occurring throughout the year and the net annual CO2 balance in the region. Thus, temporal investigations are necessary to determine natural environmental fluctuations and to distinguish natural variability from anthropogenically driven changes. We emphasize the importance of more studies regarding Cant uptake rate, accumulation, and export to global oceans.
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spelling doaj.art-5850623733524f20b835d438017b32652022-12-22T00:40:40ZengAcademia Brasileira de CiênciasAnais da Academia Brasileira de Ciências1678-26902022-05-0194suppl 110.1590/0001-3765202220210825The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectivesIOLE B.M. ORSELLIhttps://orcid.org/0000-0003-2991-292XANDRÉA C.O. CARVALHOhttps://orcid.org/0000-0002-9159-9498THIAGO MONTEIROhttps://orcid.org/0000-0001-7643-0646BRENDON Y. DAMINIhttps://orcid.org/0000-0003-4792-6057MARIAH DE CARVALHO-BORGEShttps://orcid.org/0000-0001-8766-9900CÍNTIA ALBUQUERQUEhttps://orcid.org/0000-0002-3185-328XRODRIGO KERRhttps://orcid.org/0000-0002-2632-3137Abstract Among the regions of the Southern Ocean, the northern Antarctic Peninsula (NAP) has emerged as a hotspot of climate change investigation. Nonetheless, studies have indicated issues and knowledge gaps that must be addressed to expand the understanding of the carbonate system in the region. Therefore, we focused on identifying current knowledge about sea-air CO2 fluxes (FCO2), anthropogenic carbon (Cant) and ocean acidification along NAP and provide a better comprehension of the key physical processes controlling the carbonate system. Regarding physical dynamics, we discuss the role of water masses formation, climate modes, upwelling and intrusions of Circumpolar Deep Water, and mesoscale processes. For FCO2, we show that the summer season corresponds to a strong sink in coastal areas, leading to CO2 uptake that is greater than or equal to that of the open ocean. We highlight that the prevalence of summer studies prevents comprehending processes occurring throughout the year and the net annual CO2 balance in the region. Thus, temporal investigations are necessary to determine natural environmental fluctuations and to distinguish natural variability from anthropogenically driven changes. We emphasize the importance of more studies regarding Cant uptake rate, accumulation, and export to global oceans.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652022000201119&lng=en&tlng=enCO2 fluxesanthropogenic carbonocean variabilitycarbon cycleSouthern Oceanbiogeochemistry
spellingShingle IOLE B.M. ORSELLI
ANDRÉA C.O. CARVALHO
THIAGO MONTEIRO
BRENDON Y. DAMINI
MARIAH DE CARVALHO-BORGES
CÍNTIA ALBUQUERQUE
RODRIGO KERR
The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
Anais da Academia Brasileira de Ciências
CO2 fluxes
anthropogenic carbon
ocean variability
carbon cycle
Southern Ocean
biogeochemistry
title The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
title_full The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
title_fullStr The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
title_full_unstemmed The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
title_short The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives
title_sort marine carbonate system along the northern antarctic peninsula current knowledge and future perspectives
topic CO2 fluxes
anthropogenic carbon
ocean variability
carbon cycle
Southern Ocean
biogeochemistry
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652022000201119&lng=en&tlng=en
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