Dust deposition rates extracted from a data-assimilation model of the aluminium oceanic cycle

Using dissolved aluminium (Al) data measured along 11 sections and extracted from the GEOTRACES intermediate data product (IDP2017), Xu and Weber (2021, see reference below) developed a data-assimilation model of the Al oceanic cycle. This model considers all the processes that might affect the oceanic Al distribution, i.e.: advection, diffusion, deposition of soluble Al from dust, hydrothermal sources, adsorption, desorption, uptake by diatoms, remineralization after diatom dissolution and resuspension from seafloor sediment.  Model parameters are optimized and twelve dust distributions from atmospheric models are tested to determine the patterns and rates of Al deposition that are most consistent with the GEOTRACES sections, while a range of circulation configurations are used to propagate uncertainty.  

Ultimately, the authors determined that 37.2 +/- 11 Gmol of Al must be annually added to the ocean to reproduce the data, with the Atlantic receiving significantly more soluble Al than the Indian or Pacific Oceans. Using the soluble iron:aluminium (Fe:Al) ratio observed in dust, rates of aeolian iron input to the ocean are also estimated. Globally it falls between 2.3 and 9.1 Gmol/yr, but mostly falls short of the biological Fe demand through much of the ocean.

Figure: (a) Soluble Al deposition (mmol/m2/yr) averaged across 60 optimized model configurations, weighted by their skill at reproducing GEOTRACES Al section data. Basin-integrated rates and uncertainty ranges are annotated. (b) Ratio of estimated Fe supply from dust to the Fe demand of upper ocean phytoplankton communities (estimated from satellite-derived C export and an assumed Fe:C uptake ratio). Values lower than 1 indicate that dust cannot meet the entire biological Fe demand.

Reference:

Xu, H., & Weber, T. (2021). Ocean Dust Deposition Rates Constrained in a Data‐Assimilation Model of the Marine Aluminum Cycle. Global Biogeochemical Cycles, 35(9). doi: 10.1029/2021gb007049

Latest highlights

Hydrothermal activity detected above the ultra-slow South West Indian Ridge, using a multi-proxy approach

Baudet and colleagues demonstrate the occurrence of hydrothermal venting on the Southwest Indian Ridge…

To Ba or not to Ba: Evaluating water column excess particulate barium as a proxy for water column respiration

Rahman and co-workers examine the relationship between excess particulate barium and organic matter respiration in the water column…

Assessment of the Solomon Sea’s dissolved iron contribution to the Equatorial Under Current

Sarthou and co-workers analysed 11 vertical profiles of dissolved iron at the entrance, within, and at the exit of the Solomon Sea…

Major controls on the fate of dissolved manganese in the northeastern Indian Ocean

Malla and Singh investigated the key factors controlling dissolved manganese in the northeastern Indian Ocean.

Rechercher