Machine learning approach led to the first iron climatology

Based on 32,344 dissolved iron data together with environmental predictors from contemporaneous satellite observations and reanalysis products, Huang and co-workers (2022, see reference below) propose the first data-driven surface-to-seafloor dissolved iron (Fe) climatology (1°×1°resolution). Their tools were 3 machine learning approaches among them the “random forest” method was tested as the most performant. Based on this climatology and statistical tools, the authors confirmed that atmospheric iron input plays a major role in enriching the surface tropical waters. They also show that interplay between particle remineralization, scavenging, and current transport are controlling the deep-water Fe distribution. Their analysis allows them to objectively assess the caveats and limitations of this approach. However, they eventually propose to use this climatology to evaluate the performance of the ocean biogeochemical models (OBM). With this aim, 13 process-based models are tested against data-driven climatology.

Global Dissolved Fe Dataset and Model Performance

Global Projection

Evaluation of process based Model

Figure: a) Distribution of compiled global observation dataset of dissolved Fe with the respect to surface ocean. b) Model performance evaluated with the validation dataset. c) Mean profile of dissolved Fe (dFe) with the shading representing the standard deviation. d) Mean dFe concentration at the depth between 3000 m and 3500 m in the main ocean basin. Diagrams comparing global modeled dissolved Fe from thirteen existing process-based models against the random forest data-driven model at the depth different depth intervals e) above 200 m and f) between 200 m and 600 m.


Huang, Y., Tagliabue, A., & Cassar, N. (2022). Data-Driven Modeling of Dissolved Iron in the Global Ocean. Frontiers in Marine Science9. Access the paper:10.3389/fmars.2022.837183

Latest highlights

A thorough estimate of the hydrothermal plumes on neodymium concentration and isotope oceanic cycles

Basak and coworkers investigated the influence of particulate matter on neodymium distributions in the Southern East Pacific Rise Hydrothermal Plume.

What are the drivers of the distributions of cadmium, nickel, zinc, copper and cobalt, manganese and aluminium in the Atlantic Ocean? Two papers are tackling this issue

The authors reveal that the distributions of dissolved tracers at depth in the South Atlantic are predominantly controlled by the mixing of North Atlantic Deep Water and waters of Antarctic origin…

Disentangling the sources and transport of iron in the Southern Ocean using a water mass mixing model analysis

Traill and co-workers used an extended optimum multiparameter analysis water‐mass mixing model…

A detailed investigation of iron complexation by organic ligands in the Western Tropical South Pacific Ocean

Léo Mahieu and his co-workers present the conditional concentration and binding-strength of iron-binding ligands during the GEOTRACES TONGA cruise.