Ecosystem

Geology

Subtropics

Organic chemistry

Dissolved organic carbon

Biology

Atmospheric sciences

Composite number

Mixed layer

Oceanography

Carbon fibers

Paleontology

Composite material

Chemistry

Ecology

Materials science

Biological pump

Climatology

Subduction

Tectonics

Ocean gyre

Environmental science

Flux (metallurgy)

Carbon cycle

Global Biogeochemical Cycles

Estimates of the ocean biological carbon pump are limited by uncertainties in the magnitude of the physical injection of particulate and dissolved organic carbon to the ocean interior. A major challenge is to evaluate the contribution of these physical pumps at small spatial and temporal scales (&lt;100 km and &lt;1 month). Here, we use a submesoscale permitting biophysical model covering a large domain representative of a subpolar and a subtropical gyre to quantify the impact of small‐scale physical carbon pumps.The model successfully simulates intense eddy‐driven subduction hot spots with a magnitude comparable to what has been observed in nature (1,000–6,000 mg C·m −2 ·day −1 ). These eddy‐driven subduction events are able to transfer carbon below the mixed‐layer, down to 500‐ to 1,000‐m depth. However, they contribute &lt;5% to the annual flux at the scale of the basin, due to strong compensation between upward and downward fluxes. The model also simulates hot spots of export associated with small‐scale heterogeneity of the mixed layer, which intermittently export large amounts of suspended particulate and dissolved organic carbon. The mixed‐layer pump contributes ∼20% to the annual flux. High‐resolution measurements of export flux are needed to test models such as this one and to improve our mechanistic understanding of the biological pump and how it will respond to climate change.

Effects of Eddy‐Driven Subduction on Ocean Biological Carbon Pump