The Importance of Water Mass Transport and Dissolved‐Particle Interactions on the Aluminum Cycle in the Subtropical North Atlantic

New dissolved aluminum (dAl) data from the 2017 GEOTRACES process study GApr08 along 22°N in the subtropical North Atlantic are presented. They show an east to west increase in dAl concentration in the surface waters. Simulation of these data with a 1D advection‐dust deposition revealed that, (a) ad...

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Veröffentlicht in:Global biogeochemical cycles 2021-05, Vol.35 (5), p.n/a
Hauptverfasser: Artigue, Lise, Wyatt, Neil J., Lacan, François, Mahaffey, Claire, Lohan, Maeve C.
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container_issue 5
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Wyatt, Neil J.
Lacan, François
Mahaffey, Claire
Lohan, Maeve C.
description New dissolved aluminum (dAl) data from the 2017 GEOTRACES process study GApr08 along 22°N in the subtropical North Atlantic are presented. They show an east to west increase in dAl concentration in the surface waters. Simulation of these data with a 1D advection‐dust deposition revealed that, (a) advection and dust dissolution are equally important dAl sources, (b) scavenging plays a minor role compared to advection in dAl removal, and (c) in addition to dust dissolution, another dAl source is required at the westernmost stations to fully explain our observations. We attribute this additional source to the dissolution of erosion products delivered to the western subtropical North Atlantic by the Lesser Antilles. For waters deeper than ∼200–300 m, an optimum multi‐parameter analysis allowed to separate the component of the dAl signal derived from water mass transport from its biogeochemical component. This revealed, (a) a major role played by water mass transport, (b) a net dAl removal between 200 and 800 m, attributed to scavenging at the subtropical North Atlantic scale, and (c) internal dAl inputs between 800 m and the seafloor, attributed to reversible scavenging. While the dAl oceanic distribution is usually considered to be dominated by the atmospheric dust input and removal by particle scavenging, this study highlights the important role played by advection, and the need to explicitly take this into account in order to quantitatively reveal the impact of external sources and dissolved‐particulate interactions on the Al cycle in the North Atlantic Ocean. Key Points Advection and dust deposition are the main processes driving the surface gradient of dissolved aluminum in the subtropical North Atlantic Lesser Antilles erosion products are a possible source of dissolved aluminum to the western subtropical North Atlantic Dissolved‐particle interactions play a major role in the dissolved aluminum distribution in the subtropical North Atlantic
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Key Points Advection and dust deposition are the main processes driving the surface gradient of dissolved aluminum in the subtropical North Atlantic Lesser Antilles erosion products are a possible source of dissolved aluminum to the western subtropical North Atlantic Dissolved‐particle interactions play a major role in the dissolved aluminum distribution in the subtropical North Atlantic</description><identifier>ISSN: 0886-6236</identifier><identifier>EISSN: 1944-9224</identifier><identifier>EISSN: 1944-8224</identifier><identifier>DOI: 10.1029/2020GB006569</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Advection ; Aluminium ; Aluminum ; Atmospheric particulates ; Biogeochemistry ; Dissolution ; dissolved aluminum ; Dissolving ; Dust ; Dust deposition ; Dust storms ; geochemical modeling ; GEOTRACES ; Mass transport ; Ocean floor ; Ocean, Atmosphere ; OMPA ; Particle interactions ; Removal ; reversible scavenging ; Scavenging ; Sciences of the Universe ; subtropical North Atlantic ; Surface water ; Water mass transport ; Water masses</subject><ispartof>Global biogeochemical cycles, 2021-05, Vol.35 (5), p.n/a</ispartof><rights>2021. 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This revealed, (a) a major role played by water mass transport, (b) a net dAl removal between 200 and 800 m, attributed to scavenging at the subtropical North Atlantic scale, and (c) internal dAl inputs between 800 m and the seafloor, attributed to reversible scavenging. While the dAl oceanic distribution is usually considered to be dominated by the atmospheric dust input and removal by particle scavenging, this study highlights the important role played by advection, and the need to explicitly take this into account in order to quantitatively reveal the impact of external sources and dissolved‐particulate interactions on the Al cycle in the North Atlantic Ocean. 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subjects Advection
Aluminium
Aluminum
Atmospheric particulates
Biogeochemistry
Dissolution
dissolved aluminum
Dissolving
Dust
Dust deposition
Dust storms
geochemical modeling
GEOTRACES
Mass transport
Ocean floor
Ocean, Atmosphere
OMPA
Particle interactions
Removal
reversible scavenging
Scavenging
Sciences of the Universe
subtropical North Atlantic
Surface water
Water mass transport
Water masses
title The Importance of Water Mass Transport and Dissolved‐Particle Interactions on the Aluminum Cycle in the Subtropical North Atlantic
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